TY - JOUR AU - Bezak, Vladimir AU - Ondrasova, Lenka AU - Vozar, Jan AU - Orynski, Szymon AU - Madzin, Jozef AU - Majcin, Dusan AU - Klanica, Radek AU - Bilcik, Dusan TI - Traces of collisional and transtensional processes between the Carpathia and the European platform in the geoelectric image (NE Slovakia and SE Poland) JF - ACTA GEOPHYSICA J2 - ACTA GEOPHYS PY - 2024 PG - 14 SN - 1895-6572 DO - 10.1007/s11600-023-01239-6 UR - https://m2.mtmt.hu/api/publication/34542316 ID - 34542316 N1 - Funding Agency and Grant Number: Slovak Research and Development Agency [APVV-21-0159, APVV-16-0482]; VEGA [2/0171/24] Funding text: This work was supported by the Slovak Research and Development Agency under the Contract no. APVV-21-0159, APVV-16-0482 and VEGA project 2/0171/24. We thank RNDr. Alexandra Marseni & cacute;, PhD. and Andrej Bezak for their help with the field work. AB - We present the latest magnetotelluric models on profiles in the northeastern part of Slovakia and the southeastern part of Poland. These models are focused on deciphering the tectonic structures at the contact of the Inner Carpathians with the European Platform in this area. For the Inner Carpathian block, we propose the term Carpathia. Profile SA-01 shows shallower structures and the parallel MT-05 profile shows deeper structures. These models are also correlated with the seismic profile CEL-05. All results are compatible and show an original subduction-collisional structure, which was later replaced by a transpressive-transtensional one. The most striking structures are thick highly conductive subhorizontal zones in the middle crust and a tectonically controlled deep vertical conductive structure-the Carpathian conductive zone. Other significant structures, which also appear in the seismic section, are back thrusting of Flysch Belt and the Klippen Belt basement (Penninic crust) uplift. LA - English DB - MTMT ER - TY - JOUR AU - Borleanu, F AU - Petrescu, L AU - Placinta, AO AU - Magrini, F AU - Grecu, B AU - Radulian, M AU - De Siena, L TI - Seismic attenuation tomography of Eastern Europe from ambient seismic noise analysis JF - GEOPHYSICAL JOURNAL INTERNATIONAL J2 - GEOPHYS J INT VL - 236 PY - 2024 IS - 1 SP - 547 EP - 564 PG - 18 SN - 0956-540X DO - 10.1093/gji/ggad408 UR - https://m2.mtmt.hu/api/publication/34399598 ID - 34399598 N1 - 1National Institute for Earth Physics, Măgurele, Romania Institute of Geosciences, Geophysics and Geodynamics, Johannes Gutenberg University, Mainz, D-55128, Germany Research School of Earth Sciences, Australian National University, Canberra, 2601, Australia Academy of Romanian Scientists, Bucharest, 050045, Romania Romanian Academy, Bucharest, 010071, Romania Dipartimento di Fisica e Astronomia (DIFA), Alma Mater Studiorum Università di Bologna, Bologna, 40129, Italy Export Date: 15 December 2023 AB - The Eastern-Europe region (EER), is a complex geotectonic area that captures part of the Alpine-Himalayan Orogen, the subduction of multiple NeoTethys Branches and part of the East European Craton. It is one of the most exciting geological areas in Europe due to a diversity of tectonic processes acting within it: extensional basin evolution, oceanic subduction, post-collisional volcanism, as well as active crustal deformation associated with the push of the Adria plate or the pull of the actively detaching Vrancea slab. This makes EER an excellent natural laboratory to study the behaviour of the lithosphere–asthenosphere system in a heterogeneous tectonic setting. To investigate the lateral heterogeneity and physical properties of the crust in the EER, we use ambient seismic noise data recorded by the vertical components of broad-band stations that have been operational between 1999 and 2020 in Eastern Europe and surrounding regions. We used this significant amount of data and the latest processing techniques of the ambient seismic noise field based on the continuous wavelet transform to compute cross-correlations between various station pairs, turning every available seismic station into a virtual source. The coda of the interstation cross-correlograms were used to determine coda quality factors (Qc) of Rayleigh waves in four different period ranges (3.0–5.0, 5.0–10.0, 10.0–20.0 and 20.0–30.0 s) and to invert them in the 2-D space, constructing the highest resolution attenuation tomography of the region. Our results reveal high attenuation features throughout the northeast Pannonian region, the Bohemian Massif, the East Carpathians and the Moesian Platform. Nevertheless, our findings do not emphasize a close correlation between the depth of sedimentary basins and attenuation features identified at longer periods. In addition, Qc variations are larger at short periods, indicating higher heterogeneity in the uppermost crust of Eastern Europe. Our findings demonstrate the higher efficiency of noise correlation approaches relative to earthquake data analyses investigating Qc at low frequencies. LA - English DB - MTMT ER - TY - JOUR AU - Hencz, Mátyás AU - Biró, Tamás AU - Németh, Károly AU - Szakács, Alexandru AU - Portnyagin, Maxim AU - Cseri, Zoltán AU - Pécskay, Zoltán AU - Szabó, Csaba AU - Müller, Samuel AU - Karátson, Dávid TI - Lithostratigraphy of the ignimbrite-dominated Miocene Bükk Foreland Volcanic Area (Central Europe) JF - JOURNAL OF VOLCANOLOGY AND GEOTHERMAL RESEARCH J2 - J VOLCANOL GEOTH RES VL - 445 PY - 2024 SN - 0377-0273 DO - 10.1016/j.jvolgeores.2023.107960 UR - https://m2.mtmt.hu/api/publication/34412174 ID - 34412174 N1 - Export Date: 1 January 2024 Correspondence Address: Hencz, M.; ELTE Eötvös Loránd University, Hungary; email: hencz.matyas@epss.hun-ren.hu AB - This study documents the volcanic evolution of the Miocene silicic Bükk Foreland Volcanic Area (BFVA), Northern Hungary (Central Europe) at an event-scale. The BFVA is a deeply eroded and dissected volcanic field dominated by multiple, several 10-m thick, valley-filling silicic ignimbrite units, which are chemically and texturally very similar to each other. Hence, establishing lateral correlation is a real challenge due to the sporadic and small-scale outcrops and lack of stratotypes. Detailed field observations allowed us to identify eleven lithological members including fourteen eruption events and establish a nearly complete lithostratigraphic correlation between fifteen outcrops across the BFVA. Primary pyroclastic material of each member was sampled, and volcanic glass was analyzed for major and trace element composition. The geochemical results confirm the field-based classification of the members and enable the correlation of distinct outcrops. The major and trace element composition of the glassy pyroclasts of each member of the BFVA served as basis to create a field-wide chemical reference database for regional correlational studies. Here, a new lithostratigraphic classification scheme consisting of one formation and eleven members is presented, which reflects the challenges unraveling the stratigraphy of ancient volcanic terrains. The field-based event-scale lithostratigraphy of the BFVA suggests a wet, partly sea-covered depositional environment in the close vicinity of the eruption centers providing favorable conditions to ‘fuel’ silicic explosive phreatomagmatism. On the contrary, paleosol horizons formed after almost each major eruption event or sequence suggests an overall near-coast terrestrial environment for the BFVA, where the emplacement of the pyroclastic material occurred. LA - English DB - MTMT ER - TY - JOUR AU - Bezak, Vladimir AU - Bielik, Miroslav AU - Marko, Frantisek AU - Zahorec, Pavol AU - Pasteka, Roman AU - Vozar, Jan AU - Papco, Juraj TI - Geological and tectonic interpretation of the new Bouguer gravity anomaly map of Slovakia JF - GEOLOGICA CARPATHICA J2 - GEOL CARPATH VL - 74 PY - 2023 IS - 2 SP - 109 EP - 122 PG - 14 SN - 1335-0552 DO - 10.31577/GeolCarp.2023.08 UR - https://m2.mtmt.hu/api/publication/33920037 ID - 33920037 N1 - Earth Science Institute, Slovak Academy of Sciences, Dúbravská cesta 9, P.O. Box 106, Bratislava, 840 05, Slovakia Department of Engineering Geology, Hydrology and Applied Geophysics, Faculty of Natural Sciences, Comenius University, Ilkovičova 6, 842 15, Bratislava 4, Slovakia Department of Geology and Paleontology, Faculty of Natural Sciences, Comenius University, Ilkovičova 6, Bratislava 4, 842 15, Slovakia Department of Theoretical Geodesy and Geoinformatics, Slovak University of Technology in Bratislava, Radlinského 11, Bratislava, 810 05, Slovakia Export Date: 19 January 2024 Correspondence Address: Bezák, V.; Earth Science Institute, Dúbravská cesta 9, P.O. Box 106, Slovakia; email: vladimir.bezak@savba.sk AB - This paper analyzes the latest complete Bouguer gravity anomaly map of Slovakia in relation to geological architecture. The observed gravity field consists of regional and local gravity anomalies, as well as marked horizontal gravity gradients. The most remarkable regional feature on this map is the large field with low-density masses in the northern part of Central Slovakia (the so-called Western Carpathian gravity low), which is divided into two gravity sub-lows: the Outer and Inner Western Carpathian gravity low. The source of the first sub-low is the sediments of the Outer Western Carpathian flysch units, and the second one is a crust with prevailing granites and orthogneisses. It is suggested that this field is only the torso of the original one, which stretched along the entire length of Slovakia from the SW to the NE. However, in the youngest stages of tectonic development, the negative gravity anomalous field in the territory of West and East Slovakia changed to a positive one due to the thinning of the lithosphere and crust by the influence of asthenolithic masses from the mantle. The higher density masses in Central Slovakia south of the Carpathian gravity low are not caused only by asthenolithic action. The different tectonic segment with a predominance of metamorphic complexes and a higher average density, in comparison to the low-density granitized complexes in the north, also contributes to its manifestation. The boundary between these two segments in Central Slovakia is a linear and sharp tectonic zone and coincides with the extensive Pohorela shear zone. Several local anomalies also occur on the complete Bouguer anomaly map, and they were also subjected to geological analysis. These include local areas with a predominance of heavier crust, such as the core mountains in western Slovakia, subvolcanic intrusions, metabasic complexes, and the Cadomian basements. Prominent horizontal gravity gradients reflect the tectonic interfaces (faults, shear zones) that originated mainly during the youngest period of the Western Carpathian tectonic development and were also interpreted. The faults shown in the complete Bouguer anomaly map were active mainly during the transpressional and extensional stage of the Neo-Alpine tectonic development. LA - English DB - MTMT ER - TY - JOUR AU - Brlek, M AU - Tapste, RS AU - Schindlbeck-Belo, J AU - Gaynor, SP. AU - Kutterolf, S AU - Hauff, F AU - Georgiev, SV. AU - Trinajstić, N AU - Šuica, S AU - Brčić, V AU - Wang, KL AU - Lee, HY AU - Beier, C AU - Abersteiner, AB. AU - Mišur, I AU - Peytcheva, I AU - Kukoč, D AU - Németh, Bianka AU - Trajanova, M AU - Balen, D AU - Guillong, M AU - Szymanowski, D AU - Haranginé Lukács, Réka TI - Tracing widespread Early Miocene ignimbrite eruptions and petrogenesis at the onset of the Carpathian-Pannonian Region silicic volcanism JF - GONDWANA RESEARCH J2 - GONDWANA RES VL - 116 PY - 2023 SP - 40 EP - 60 PG - 21 SN - 1342-937X DO - 10.1016/j.gr.2022.12.015 UR - https://m2.mtmt.hu/api/publication/33539754 ID - 33539754 AB - The Carpathian-Pannonian Region (CPR) hosted some of the largest silicic volcanic eruptions in Europe during the Early and Middle Miocene, contemporaneously with major lithospheric thinning of the Pannonian Basin. This was recorded as an ignimbrite flare-up event from approximately 18.1–14.4 Ma. To gain in-depth perspectives on the eruption chronology, tephrostratigraphy, and petrogenesis at the onset of CPR silicic volcanism, we applied a multi-proxy approach to Lower Miocene rhyolitic ignimbrites and pyroclastic fall deposits from the northern CPR to the Dinaride Lake System. High-precision zircon U-Pb geochronology distinguished two Lower Miocene groups of volcaniclastic rocks at ∼18.1 Ma and ∼17.3 Ma. Based on combined tephrostratigraphic signatures we propose that the ∼18.1 Ma Kalnik and ∼17.3 Ma Eger eruptions produced widespread (intermediate to) large caldera-forming massive rhyolitic ignimbrites, deposited across northern and southwestern regions of the CPR. Due to easterly winds that carried volcanic ash hundreds of kilometers to the southwest, Eger eruption products also reached distal intra-montane Dinaride lacustrine basins, recorded as pyroclastic fall deposits. Heterogeneous major and trace elemental compositions of ∼18.1 Ma volcanic glass shards suggest that the Kalnik eruption was sourced from complex silicic magmatic systems, with simultaneous tapping of two discrete melt bodies during the eruption. The homogeneous geochemical composition of ∼17.3 Ma glasses is distinct from the older glasses. Integrated zircon and bulk glass Nd-Hf isotope compositions have a positive correlation, defining a regional mantle array, and are more radiogenic in the younger phase of volcanism. The recorded systematic isotopic change, moving from older more crustal signatures to younger more juvenile compositions, imply that during the period of lithospheric thinning of the Pannonian Basin the region underwent more complex variations in the interaction between metasomatized lithospheric mantle-derived magmas and various crustal components than previously recognized. LA - English DB - MTMT ER - TY - JOUR AU - Harangi, Szabolcs AU - Szarvas, I AU - Haranginé Lukács, Réka TI - Wide-ranging and violent volcanic history of a quiet transborder area : volcanic geoheritage of the Novohrad–Nógrád UNESCO Global Geopark JF - GEOCONSERVATION RESEARCH J2 - GEOCONSERVATION RES VL - 6 PY - 2023 IS - 1 SP - 178 EP - 206 PG - 29 SN - 2588-7343 DO - 10.30486/gcr.2023.1982587.1133 UR - https://m2.mtmt.hu/api/publication/34052385 ID - 34052385 N1 - Eötvös Loránd University, Faculty of Geography and Earth Sciences, Department of Petrology and Geochemsitry, Pázmány sétány 1/C, Budapest, H-1117, Hungary MTA-ELTE Volcanology Research Group, Pázmány sétány 1/C, Budapest, H-1117, Hungary Ipolytarnóc Fossils Nature Conservation Area, Bükk National Park, Ipolytarnóc, Hungary Institute for Geological and Geochemical Research, Research Centre for Astronomy and Earth Sciences, Eötvös Loránd Research Network (ELKH), Budapest, Hungary Cited By :1 Export Date: 13 October 2023 Correspondence Address: Harangi, S.; Eötvös Loránd UniversityHungary; email: harangi.szabolcs@ttk.elte.hu AB - The Novohrad–Nógrád UNESCO Global Geopark is the first cross-border geopark located between Slovakia and Hungary, Eastern–Central Europe. “Ancient world without borders” – its motto reflects both the remarkable geodiversity and the strong link between people living on either side of the state border. In this relatively small area, almost all types of eruption products can be found from basaltic through andesitic to rhyolitic, reflecting the wide-ranging volcanism of the Pannonian Basin over the last 20 million years, which were the largest eruptions in Europe at the time. The Ipolytarnóc Site, the gateway of the geopark and possessor of a European- Diploma for Protected Areas, documents when one of these devastating eruption events buried a subtropical-forested area with thick pyroclastic deposits and preserved vertebrate footprints. On the other hand, relatively young eruptions of basaltic magmas occurred in this area that give another specific atmosphere to the geopark. Columnar jointing with concave and convex curvilinear shapes shown both by basalts and andesites is another peculiar natural value. Due to the regional uplift and the associated erosion, most of the volcanic edifices were removed and the root zones of the volcanoes were revealed, giving a special character. The volcanic heritage meets specific cultural and historical heritage, which makes this geopark a particular tourist destination. There are four visitor centers and several nature trails with explanation panels showing concise summaries of the volcanological features in three languages (Hungarian, Slovakian and English). Among the rich indoor and outdoor activities, the annual Volcano Day program in Ipolytarnóc with an interactive volcano show attracts many people. This is an evolving geopark, where continuously renewing attractions serve the geoeducation and geotourism purposes in parallel with geoheritage conservation management. LA - English DB - MTMT ER - TY - JOUR AU - Hencz, Mátyás AU - Biró, Tamás AU - Németh, Károly AU - Porkoláb, Kristóf AU - Kovács, István János AU - Spránitz, Tamás AU - Cloetingh, Sierd AU - Szabó, Csaba AU - Berkesi, Márta TI - Tectonically-determined distribution of monogenetic volcanoes in a compressive tectonic regime: An example from the Pannonian continental back-arc system (Central Europe) JF - JOURNAL OF VOLCANOLOGY AND GEOTHERMAL RESEARCH J2 - J VOLCANOL GEOTH RES VL - 444 PY - 2023 SP - 107940 PG - 18 SN - 0377-0273 DO - 10.1016/j.jvolgeores.2023.107940 UR - https://m2.mtmt.hu/api/publication/34210603 ID - 34210603 N1 - MTA-EPSS FluidsByDepth Lendület Research Group, Institute of Earth Physics and Space Science, Hungarian Research Network, Sopron, Hungary Department of Physical Geography, Institute of Geography and Earth Sciences, ELTE Eötvös Loránd University, Budapest, Hungary National Program for Earthquakes and Volcanoes, Geohazard Research Center, Saudi Geological Survey, Jeddah, Saudi Arabia Istituto Nazionale di Geofisica e Vulcanologia, Bologna, Italy MTA-EPSS Lendület Pannon LitH2Oscope Research Group, Institute of Earth Physics and Space Science, Hungarian Research Network, Sopron, Hungary Lithosphere Fluid Research Lab, Institute of Geography and Earth Sciences, Eötvös Loránd University, Budapest, Hungary Tectonics Research Group, Department of Earth Sciences, Utrecht University, Netherlands Export Date: 30 November 2023 Correspondence Address: Hencz, M.; MTA-EPSS FluidsByDepth Lendület Research Group, Hungary; email: hencz.matyas@epss.hun-ren.hu AB - This paper presents the results from a geographic information systems (GIS) workflow, which was used to analyze the spatial distribution and temporal evolution of volcanoes in the Mio-Pleistocene monogenetic Bakony-Balaton Highland Volcanic Field (BBHVF), located in the Pannonian Basin, Hungary. Volcanism occurred during the tectonic inversion in a back-arc setting and a compressive/transpressive tectonic regime on the hottest and thinnest lithosphere of continental Europe. The main goal of this study is to clarify the effect of the pre-existing structure of the upper lithosphere in the distribution of the volcanic centers across the volcanic field using an innovative GIS methodology. Orientation of the volcanic field was compared to the orientation of the faults in the BBHVF, and in its larger vicinity, which resulted in correspondence, suggesting the dominance of the SW-NE direction. The directions of the volcanic lineaments fit well to the two main fault directions. The fault-volcano proximity analysis suggests that the fault plane of a thrust fault was an important structural feature during the lifespan of the volcanism. All results suggest that the fault plane of a regionally significant Cretaceous thrust fault (Litér Fault) might have likely served as a temporary pathway for the ascending magma, whereby (similarly to other, smaller faults) redirecting the magmas causing clustering of the volcanoes. This highlights the importance of major upper crustal structural heterogeneities for magma transport in a compressive tectonic system, especially in the case of active, monogenetic volcanic fields from a volcanic hazard perspective. The present GIS workflow can be effective in analyzing the spatial patterns of the volcanism and its connection with crustal structures at monogenetic volcanic fields worldwide. LA - English DB - MTMT ER - TY - JOUR AU - Kelemen, Péter AU - Dunkl, István AU - Csillag, Gábor AU - Mindszenty, Andrea AU - Józsa, Sándor AU - Fodor, László AU - von Eynatten, Hilmar TI - Origin, timing and paleogeographic implications of Paleogene karst bauxites in the northern Transdanubian range, Hungary JF - INTERNATIONAL JOURNAL OF EARTH SCIENCES J2 - INT J EARTH SCI VL - 112 PY - 2023 IS - 1 SP - 243 EP - 264 PG - 22 SN - 1437-3254 DO - 10.1007/s00531-022-02249-3 UR - https://m2.mtmt.hu/api/publication/33126810 ID - 33126810 N1 - Funding Agency and Grant Number: Eotvos Lorand University Funding text: Open access funding provided by Eotvos Lorand University. AB - Paleogene karst bauxites in the northeastern Transdanubian Range and their cover sequences provide valuable sedimentary archives, despite their weathered nature and vague paleontological records. U–Pb detrital zircon geochronology combined with heavy mineral analysis indicates ‘local’ Alpine aeolian and fluvial sources and ‘distant’ aeolian sources connected to the Bohemian Massif. Records of episodic Paleogene volcanic eruptions related to igneous complexes of the Adamello and probably also the Bergell, Recsk and Balkan Peninsula, are reflected by euhedral zircon crystals. Their U–Pb geochronology supplies age constraints for the phases of subaerial exposure of the karstic surface and the accumulation of bauxitic protoliths and helps to improve the existing stratigraphic records and to define stages of denudation in the northeastern Transdanubian Range. Distinct phases of subaerial exposure and accumulation of the bauxite's protoliths are identified as ca. 42, 35 and 31 Ma; alternating with episodes of subsidence, represented by siliciclastic and carbonatic sequences at ca. 38, 32 and 31 Ma. Besides Paleogene volcanism, zircon dating also revealed contributions from the Middle Triassic tuffs of the Transdanubian Range. Garnet, epidote, kyanite, staurolite, and xenotime/monazite crystals suggest fluvial drainage of diverse metamorphic units of the Austroalpine basement from the Eastern- and Southern Alps, which also supplied most of the pre-Mesozoic zircons. However, the unexpectedly high proportion of Variscan ages in the bauxites most likely relate to igneous rocks of the Bohemian Massif, thus suggesting additional long-distance aeolian sources. The new data allow for detailed reconstructions of the Paleogene evolution and palaeogeography of the northeastern Transdanubian range. LA - English DB - MTMT ER - TY - JOUR AU - Mihályka, János AU - Paróczi, Petra AU - Balázs, László AU - Drahos, Dezső AU - Lenkey, László TI - Thermal Conductivity of Sediments from Well-Logs and its Application to Determine Heat Flow Density in the Pannonian Basin, Hungary JF - TECTONOPHYSICS J2 - TECTONOPHYSICS VL - 868 PY - 2023 PG - 16 SN - 0040-1951 DO - 10.1016/j.tecto.2023.230095 UR - https://m2.mtmt.hu/api/publication/34145447 ID - 34145447 N1 - Export Date: 15 December 2023 Correspondence Address: Mihályka, J.; Department of Geophysics and Space Sciences, Pázmány Péter stny 1/C, Hungary; email: mihalyka.janos@ttk.elte.hu LA - English DB - MTMT ER - TY - JOUR AU - Roger, Marion AU - de Leeuw, Arjan AU - van der Beek, Peter AU - Husson, Laurent AU - Sobel, Edward R. AU - Glodny, Johannes AU - Bernet, Matthias TI - Construction of the Ukrainian Carpathian wedge from low-temperature thermochronology and tectono-stratigraphic analysis JF - SOLID EARTH J2 - SOLID EARTH VL - 14 PY - 2023 IS - 2 SP - 153 EP - 179 PG - 27 SN - 1869-9510 DO - 10.5194/se-14-153-2023 UR - https://m2.mtmt.hu/api/publication/33850430 ID - 33850430 N1 - Institut des Sciences de la Terre (ISTerre), Université Grenoble Alpes, CNRS, IRD, Grenoble, 38000, France Institut für Geowissenschaften, Universität Potsdam, Potsdam, 14476, Germany GFZ German Research Centre for Geosciences, Potsdam, 14473, Germany Export Date: 3 January 2024 Correspondence Address: Roger, M.; Institut des Sciences de la Terre (ISTerre), France; email: marion.roger@univ-grenoble-alpes.fr AB - The evolution of orogenic wedges can be determined through stratigraphic and thermochronological analysis. We used apatite fission-track (AFT) and apatite and zircon (U-Th-Sm) / He (AHe and ZHe) low-temperature thermochronology to assess the thermal evolution of the Ukrainian Carpathians, a prime example of an orogenic wedge forming in a retreating subduction zone setting. Whereas most of our AHe ages are reset by burial heating, 8 out of 10 of our AFT ages are partially reset, and none of the ZHe ages are reset. We inverse-modeled our thermochronology data to determine the time-temperature paths of six of the eight nappes composing the wedge. The models were integrated with burial diagrams derived from the stratigraphy of the individual nappes, which allowed us to distinguish sedimentary from tectonic burial. This analysis reveals that accretion of successive nappes and their subsequent exhumation mostly occurred sequentially, with an apparent increase in exhumation rate towards the external nappes. Following a phase of tectonic burial, the nappes were generally exhumed when a new nappe was accreted, whereas, in one case, duplexing resulted in prolonged burial. An early orogenic wedge formed with the accretion of the innermost nappe at 34 Ma, leading to an increase in sediment supply to the remnant basin. Most of the other nappes were accreted between 28 and 18 Ma. Modeled exhumation of the outermost nappe started at 12 Ma and was accompanied by out-of-sequence thrusting. The latter was linked to emplacement of the wedge onto the European platform and consequent slab detachment. The distribution of thermochronological ages across the wedge, showing non-reset ages in both the inner and outer part of the belt, suggests that the wedge was unable to reach dynamic equilibrium for a period long enough to fully reset all thermochronometers. Non-reset ZHe ages indicate that sediments in the inner part of the Carpathian embayment were mostly supplied by the Inner Carpathians, while sediments in the outer part of the basin were derived mostly from the Teisseyre-Tornquist Zone (TTZ) or the southwestern margin of the East European Platform. Our results suggest that during the accretionary phase, few sediments were recycled from the wedge to the foredeep. Most of the sediments derived from the Ukrainian Carpathian wedge were likely transported directly to the present pro- and retro-foreland basins. LA - English DB - MTMT ER - TY - JOUR AU - Trinajstić, N AU - Brlek, M AU - Gaynor, SP. AU - Schindlbeck-Belo, J AU - Šuica, S AU - Avanić, R AU - Kutterolf, S AU - Wang, KL AU - Lee, HY AU - Holcová, K AU - Kopecká, J AU - Baranyi, V AU - Hajek-Tadesse, V AU - Bakrač, K AU - Brčić, V AU - Kukoč, D AU - Milošević, M AU - Mišur, I AU - Haranginé Lukács, Réka TI - Provenance and depositional environment of Middle Miocene silicic volcaniclastic deposits from Mt. Medvednica (North Croatian Basin, Carpathian-Pannonian Region) JF - JOURNAL OF VOLCANOLOGY AND GEOTHERMAL RESEARCH J2 - J VOLCANOL GEOTH RES VL - 443 PY - 2023 SN - 0377-0273 DO - 10.1016/j.jvolgeores.2023.107917 UR - https://m2.mtmt.hu/api/publication/34153996 ID - 34153996 N1 - Croatian Geological Survey, Department of Geology, Sachsova 2, HR-10000, Zagreb, Croatia University of Geneva, Department of Earth Sciences, Rue des Maraichers 13, Geneva, 1205-CH, Switzerland Department of Geosciences, Guyot Hall, Princeton UniversityNJ 08544, United States GEOMAR Helmholtz Center for Ocean Research Kiel, FB4, Dynamics of the Ocean Floor, Wischhofstrasse 1-3, Kiel, D-24148, Germany INA-Industrija nafte, d.d., Exploration and Production Laboratory, Lovinčićeva 4, HR-10000, Zagreb, Croatia Institute of Earth Sciences, Academia Sinica, 128 Academia Road Sec. 2, Nangang, Taipei, 115, Taiwan Department of Geosciences, National Taiwan University, No. 1, Sec. 4, Roosevelt Rd, Taipei, 10617, Taiwan Institute of Geology and Palaeontology, Charles University, Albertov 6, Prague 2, 128 43, Czech Republic Palacký University, Department of Biology, Faculty of Education, Purkrabská 2, Olomouc, 779 00, Czech Republic MTA-ELTE Volcanology Research Group, Budapest Pázmány Péter sétány 1/C, Budapest, 1117, Hungary Institute for Geological and Geochemical Research, Research Centre for Astronomy and Earth Sciences (MTA Centre of Exellence), Eötvös Loránd Research Network (ELKH), Budaörsi út 45, Budapest, H-1112, Hungary Export Date: 31 October 2023 Correspondence Address: Brlek, M.; Croatian Geological Survey, Sachsova 2, HR-10000, Croatia; email: mihovil.brlek@hgi-cgs.hr LA - English DB - MTMT ER - TY - JOUR AU - Babejová-Kmecová, J. AU - Plašienková, I. AU - Sliva, L. AU - Halásová, E. AU - Hudácková, N. TI - From dysoxic sea to hypersaline lagoon: Paleoenvironmental changes on the Badenian/Sarmatian boundary (borehole MZ102; Vienna basin) JF - ACTA GEOLOGICA SLOVACA J2 - ACTA GEOL SLOV VL - 14 PY - 2022 IS - 1 SP - 57 EP - 72 PG - 16 SN - 1338-0044 UR - https://m2.mtmt.hu/api/publication/33189026 ID - 33189026 N1 - Univerzita Komenského, Prírodovedecká Fakulta, Katedra Geológie A Paleontológie, Ilkovicova 6, Bratislava, 842 15, Slovakia Nafta A. S., Bratislava, 821 09, Slovakia Cited By :1 Export Date: 8 May 2023 LA - English DB - MTMT ER - TY - JOUR AU - Bielik, Miroslav AU - Zeyen, Herman AU - Starostenko, Vitaly AU - Makarenko, Irina AU - Legostaeva, Olga AU - Savchenko, Sasha AU - Dérerová, Jana AU - Grinč, Michal AU - Godová, Dominika AU - Pánisová, Jaroslava TI - A review of geophysical studies of the lithosphere in the Carpathian–Pannonian region JF - GEOLOGICA CARPATHICA J2 - GEOL CARPATH VL - 73 PY - 2022 IS - 6 SP - 499 EP - 516 PG - 18 SN - 1335-0552 DO - 10.31577/GeolCarp.73.6.2 UR - https://m2.mtmt.hu/api/publication/33541001 ID - 33541001 N1 - Earth Science Institute, Slovak Academy of Sciences, Dúbravská cesta 9, P.O. Box 106, Bratislava, 840 05, Slovakia Department of Engineering Geology, Hydrology and Applied Geophysics, Faculty of Natural Sciences, Comenius University, Ilkovičova 6, Bratislava, 842 15 4, Slovakia Department des Sciences de la Terre Universite de Paris-Saclay, Bat. 504, Orsay, Cedex F-91405, France Institute of Geophysics National Academy of Sciences of Ukraine, Palladin, av. 32, Kiev, 03680, Ukraine INSET s.r.o., Lucemburská 1170/7, Praha 3, 130 00, Czech Republic Export Date: 27 January 2023 Correspondence Address: Bielik, M.; Earth Science Institute, Dúbravská cesta 9, P.O. Box 106, Slovakia; email: bielik@fns.uniba.sk LA - English DB - MTMT ER - TY - JOUR AU - Catlos, EJ. AU - Broska, I AU - Kohút, M AU - Etzel, TM. AU - Kyle, JR AU - Stockli, DF. AU - Miggins, DP AU - Campos, D TI - Geochronology, geochemistry, and geodynamic evolution of Tatric granites from crystallization to exhumation (Tatra Mountains, Western Carpathians) JF - GEOLOGICA CARPATHICA J2 - GEOL CARPATH VL - 73 PY - 2022 IS - 6 SP - 517 EP - 544 PG - 28 SN - 1335-0552 DO - 10.31577/GeolCarp.73.6.1 UR - https://m2.mtmt.hu/api/publication/33535625 ID - 33535625 N1 - Department of Geological Sciences, Jackson School of Geosciences, The University of Texas at Austin, Austin, TX 78712, United States Earth Science Institute of the Slovak Academy of Sciences, Dúbravská cesta 9, Bratislava, 840 05, Slovakia ExxonMobil, 22777 Springwoods Village Parkway, Spring, TX 77389, United States College of Earth, Ocean, and Atmospheric Sciences, Oregon State University, 104 CEOAS Admin Bldg., Corvallis, OR 97331-5503, United States Export Date: 14 February 2023 Correspondence Address: Catlos, E.J.; Department of Geological Sciences, United States; email: ejcatlos@jsg.utexas.edu LA - English DB - MTMT ER - TY - JOUR AU - Erdős, Zoltán AU - Huismans, RS AU - Faccenna, C TI - Wide Versus Narrow Back-Arc Rifting: Control of Subduction Velocity and Convective Back-Arc Thinning JF - TECTONICS J2 - TECTONICS VL - 41 PY - 2022 IS - 6 SN - 0278-7407 DO - 10.1029/2021TC007086 UR - https://m2.mtmt.hu/api/publication/32930743 ID - 32930743 N1 - Funding Agency and Grant Number: Hungarian National Research Fund project [OTKA-K120149] Funding text: This work has been carried out by the financial support of the Hungarian National Research Fund project OTKA-K120149. The authors thank Uninett Sigma2 for computing time of project NN4704K. The authors would like to thank Laurent Jolivet for his excellent editorial work as well as the three anonymous reviewers for their constructive comments. LA - English DB - MTMT ER - TY - JOUR AU - Gandhi, Arun AU - Bartók, Blanka AU - Musyimi, Peter Kinyae AU - Ilona, Judit AU - Weidinger, Tamás TI - Historical fog climate dataset for Carpathian Basin from 1886 to 1919 JF - DATA IN BRIEF J2 - DATA BRIEF VL - 44 PY - 2022 SN - 2352-3409 DO - 10.1016/j.dib.2022.108500 UR - https://m2.mtmt.hu/api/publication/33037042 ID - 33037042 N1 - Funding Agency and Grant Number: Hungarian government; [GINOP2.3.2-15-2016-00007]; [GINOP-2.3.2-15-2016-00055]; [OTKA-138176] Funding text: The research was supported by 'GINOP2.3.2-15-2016-00007, GINOP-2.3.2-15-2016-00055, OTKA-138176'. The Stipendium Hungaricum doctoral research scholarship of the Hungarian government has financially supported Arun Gandhi's work. We are grateful to Agoston Vilmos Tordai for providing us help in decoding the symbols depicted in the yearbooks LA - English DB - MTMT ER - TY - JOUR AU - Golonka, Jan AU - Waskowska, Anna AU - Cichostepski, Kamil AU - Dec, Jerzy AU - Pietsch, Kaja AU - Loj, Monika AU - Bania, Grzegorz AU - Moscicki, Wlodzimierz Jerzy AU - Porzucek, Slawomir TI - Melange, Flysch and Cliffs in the Pieniny Klippen Belt (Poland): An Overview JF - MINERALS J2 - MINERALS-BASEL VL - 12 PY - 2022 IS - 9 PG - 28 SN - 2075-163X DO - 10.3390/min12091149 UR - https://m2.mtmt.hu/api/publication/33167952 ID - 33167952 N1 - Export Date: 2 January 2023 Correspondence Address: Golonka, J.; Faculty of Geology, al. Mickiewicza 30, Poland; email: jgolonka@agh.edu.pl AB - The Pieniny Klippen Belt (PKB) is located in the suture zone between the Central and Outer (Flysch) Carpathians. Its structure is an effect of prolonged processes of the Cretaceous-Miocene folding, thrusting and uplifting. In this zone, tectonic components of different ages and features, including strike-slip-bounded tectonic blocks, thrust units, as well as toe-thrusts and olistostromes, result in the present-day melange characteristics of the PKB, where individual tectonic units are difficult to distinguish. In the PKB, both tectonic and sedimentary events triggered the melange creation. The name "Klippen Belt" is derived from cliffs (German Klippen). These cliffs form harder, more erosion-resistant elements of the melange, residing within less competent clastic deposits, sandstones, shales and marls that form flysch complexes. The cliffs often represent olistoliths, which glided down from elevated areas to the deeper basinal zones. Two olistostrome belts were distinguished. The older one resulted from subduction of the southern part of the Alpine Tethys, and the younger originated in response to the northward shift of the accretionary wedge. The other cliffs were placed within the surrounding clastic by tectonic deformational processes. The flower structure of the PKB was formed during the collision and strike-slip movement of the lithospheric plates. This structure is limited on both sides by deep-rooted faults. Several evolutionary stages could be distinguished in these areas. The rift-related stage is expressed by the opening of the Alpine Tethys that contains two major basins-Magura and Pieniny (Zlatne) basins, separated by Czorsztyn Ridge. The reorganization of the Alpine Tethys basins and the development of the accretionary prism happened during the synorogenic stage. This process was initiated by the movement of the Central Carpathians. Thick flysch sequences with olistostromes were deposited in these basins. The Czorsztyn Ridge was destroyed during the late orogenic stages. LA - English DB - MTMT ER - TY - JOUR AU - Krstekanić, Nemanja AU - Matenco, Liviu AU - Stojadinovic, Uros AU - Willingshofer, Ernst AU - Toljić, Marinko AU - Tamminga, Daan TI - Strain partitioning in a large intracontinental strike-slip system accommodating backarc-convex orocline formation: The Circum-Moesian Fault System of the Carpatho-Balkanides JF - GLOBAL AND PLANETARY CHANGE J2 - GLOBAL PLANET CHANGE VL - 208 PY - 2022 SN - 0921-8181 DO - 10.1016/j.gloplacha.2021.103714 UR - https://m2.mtmt.hu/api/publication/32529867 ID - 32529867 N1 - Funding Agency and Grant Number: Netherlands Research Centre for Integrated Solid Earth Science (ISES) Funding text: This paper is part of a collaboration between the Department of Earth Sciences at Utrecht University, the Netherlands and the Faculty of Mining and Geology, University of Belgrade, Serbia during the PhD of Nemanja Krstekanic and is funded by the Netherlands Research Centre for Integrated Solid Earth Science (ISES). We thank Timotije Tufegdzic for his help during the fieldwork. Djordje Grujic is gratefully acknowledged for helpful discussions and suggestions on an earlier version of the manuscript. We thank Editor Zhengtang Guo and two anonymous reviewers for their constructive comments and suggestions, which have significantly improved the original version of the manuscript. LA - English DB - MTMT ER - TY - JOUR AU - Haranginé Lukács, Réka AU - Harangi, Szabolcs AU - Gál, Péter AU - Szepesi, János AU - Di Capua, A AU - Norini, G AU - Sulpizio, R AU - Groppelli, G AU - Fodor, László TI - Formal definition and description of lithostratigraphic units related to the Miocene silicic pyroclastic rocks outcropping in Northern Hungary: a revision JF - GEOLOGICA CARPATHICA J2 - GEOL CARPATH VL - 73 PY - 2022 IS - 2 SP - 137 EP - 158 PG - 22 SN - 1335-0552 DO - 10.31577/GeolCarp.73.2.3 UR - https://m2.mtmt.hu/api/publication/32787471 ID - 32787471 N1 - Institute for Geological and Geochemical Research, Research Centre for Astronomy and Earth Sciences, Eötvös Loránd Research Network (ELKH), Budaörsi út 45, Budapest, 1112, Hungary MTA-ELTE Volcanology Research Group, Eötvös Loránd Research Network (ELKH), Pázmány P. sétány 1/C, Budapest, 1117, Hungary Eötvös Loránd University, Institute of Geography and Earth Sciences, Department of Petrology and Geochemistry, Pázmány P. s. 1/C, Budapest, 1117, Hungary Isotope Climatology and Environmental Research Centre (ICER), Institute for Nuclear Research, ELKH, Debrecen, Hungary CNR IGAG, Institute of Environmental Geology and Geoengineering, Via M. Bianco 9, Milan, 20131, Italy University of Bari “Aldo Moro”, Department of Earth and Geoenvironmental Sciences, Via Orabona 4, Bari, 70125, Italy Eötvös Loránd University, Institute of Geography and Earth Sciences, Department of Geology, Pázmány P. s. 1/C, Budapest, 1117, Hungary ELKH-ELTE Geological, Geophysical and Space Science Research Group, Eötvös Loránd Research Network (ELKH), Pázmány P. sétány 1/C, Budapest, 1117, Hungary Export Date: 17 June 2022 Correspondence Address: Lukács, R.; Institute for Geological and Geochemical Research, Budaörsi út 45, Hungary; email: lukacs.reka@csfk.org LA - English DB - MTMT ER - TY - JOUR AU - Myšľan, P. AU - Števko, M. AU - Sejkora, J. AU - Dolníček, Z. TI - Dachiardite-Ca, ferrierite-Mg and associated zeolite mineralization in chalcedony cavities from localities Byšta, Brezina and Kuzmice (Slanské vrchy Mts., Slovak Republic) JF - Bulletin Mineralogie Petrologie J2 - Bull Mineral Petrolog VL - 30 PY - 2022 IS - 1 SP - 45 EP - 60 PG - 16 SN - 2570-7337 DO - 10.46861/bmp.30.045 UR - https://m2.mtmt.hu/api/publication/34518697 ID - 34518697 N1 - Ústav vied o Zemi Slovenskej akadémie vied, v.v.i., Dúbravská cesta 9, P. O. BOX 106, Bratislava, 840 05, Slovakia Katedra mineralógie, petrológie a ložiskovej geológie, Prírodovedecká fakulta, Univerzita Komenského v Bratislave, Ilkovičova 6, Mlynská dolina, Bratislava, 842 15, Slovakia Mineralogicko-petrologické oddělení, Národní muzeum, Cirkusová 1740, Horní Počernice, Praha 9, 193 00, Czech Republic Export Date: 19 January 2024 Correspondence Address: Myšľan, P.; Ústav vied o Zemi Slovenskej akadémie vied, Dúbravská cesta 9, P. O. BOX 106, Slovakia; email: myslan.pavol@gmail.com LA - Slovak DB - MTMT ER - TY - JOUR AU - Pezzo, G. AU - Palano, M. AU - Chiarabba, C. TI - Rotation at subduction margins: How complexity at fault-scale (the 2019 Albanian Mw 6.4 earthquake) mirrors the regional deformation JF - TERRA NOVA J2 - TERRA NOVA VL - 34 PY - 2022 IS - 3 SP - 244 EP - 252 PG - 9 SN - 0954-4879 DO - 10.1111/ter.12584 UR - https://m2.mtmt.hu/api/publication/32915030 ID - 32915030 N1 - Istituto Nazionale di Geofisica e Vulcanologia, Osservatorio Nazionale Terremoti, Rome, Italy Istituto Nazionale di Geofisica e Vulcanologia, Osservatorio Etneo - Sezione di Catania, Catania, Italy Export Date: 1 July 2022 Correspondence Address: Pezzo, G.; Istituto Nazionale di Geofisica e Vulcanologia, Italy; email: giuseppe.pezzo@ingv.it LA - English DB - MTMT ER - TY - JOUR AU - Szakács, A AU - Kovacs, M TI - Volcanic Landforms and Landscapes of the East Carpathians (Romania) and Their Geoheritage Values JF - LAND (BASEL) J2 - LAND-BASEL VL - 11 PY - 2022 IS - 7 PG - 40 SN - 2073-445X DO - 10.3390/land11071064 UR - https://m2.mtmt.hu/api/publication/33025440 ID - 33025440 LA - English DB - MTMT ER - TY - JOUR AU - Tamás, Csibri AU - Andrej, Ruman AU - Natalia, Hudackova AU - Michal, Jamrich AU - L'ubomir, Sliva AU - Katarína, Šarinová AU - Michal, Kovac TI - Deltaic systems of the northern Vienna Basin: The lower-middle Miocene conglomerate bodies JF - GEOLOGICA CARPATHICA J2 - GEOL CARPATH VL - 73 PY - 2022 IS - 3 SP - 245 EP - 269 PG - 25 SN - 1335-0552 DO - 10.31577/GeolCarp.73.3.5 UR - https://m2.mtmt.hu/api/publication/32893701 ID - 32893701 N1 - NAFTA a.s., Exploration and Production, Plavecký Štvrtok 900, Plavecký Štvrtok900 68, Slovakia Department of Geology and Paleontology, Faculty of Natural Sciences, Comenius University Bratislava, Mlynská dolina, Ilkovičova 6, Bratislava, 842 15, Slovakia Department of Mineralogy and Petrology, Faculty of Natural Sciences, Comenius University Bratislava, Mlynská dolina, Ilkovičova 6, Bratislava, 842 15, Slovakia Export Date: 26 August 2022 Correspondence Address: Csibri, T.; NAFTA a.s., Plavecký Štvrtok 900, Plavecký Štvrtok, Slovakia; email: tamas.csibri@nafta.sk LA - English DB - MTMT ER - TY - CHAP AU - Vojtko, R AU - Plašienka, D AU - Kováč, M ED - Lehotský, Milan ED - Boltižiar, Martin TI - Outline of Geology and Cenozoic Evolution of Slovakia T2 - Landscapes and Landforms of Slovakia PB - Springer Netherlands CY - Cham SN - 9783030892937 T3 - World Geomorphological Landscapes, ISSN 2213-2090 PY - 2022 SP - 9 EP - 26 PG - 18 DO - 10.1007/978-3-030-89293-7_2 UR - https://m2.mtmt.hu/api/publication/32825822 ID - 32825822 N1 - Export Date: 30 June 2022 Correspondence Address: Vojtko, R.; Department of Geology and Palaeontology, Ilkovičova 6, Slovakia; email: rastislav.vojtko@uniba.sk LA - English DB - MTMT ER - TY - JOUR AU - Bezak, Vladimir AU - Vozar, Jan AU - Majcin, Dusan AU - Klanica, Radek AU - Madaras, Jan TI - Contrasting tectonic styles of the western and eastern parts of the Western Carpathian Klippen Belt in Slovakia based on magnetotelluric sounding of deep tectonic structures JF - GEOLOGICAL QUARTERLY J2 - GEOL Q VL - 65 PY - 2021 IS - 2 PG - 11 SN - 1641-7291 DO - 10.7306/gq.1595 UR - https://m2.mtmt.hu/api/publication/32272626 ID - 32272626 N1 - Slovak Academy of Sciences, Earth Science Institute, Dúbravská 9, Bratislava, 840 05, Slovakia Institute of Geophysics, Czech Academy of Sciences, Boční II/1401, Praha 4, 141 31, Czech Republic Export Date: 1 July 2022 Correspondence Address: Bezák, V.; Slovak Academy of Sciences, Dúbravská 9, Slovakia; email: geofbezv@savba.sk AB - To characterize the deep structure of the Klippen Belt, we made magnetotelluric measurements in profiles across the western and eastern segments in the territory of Slovakia, from which we created 3D models. The models revealed significant differences in tectonic structure between these segments. In the western segment, the Klippen Belt is located in the southern reversing wing of the original subduction flower structure (retroarc thrusting) with an overthrust to the south onto the Inner Western Carpathian units. This structure was later modified by significant transpressional movements. In the eastern segment, the Klippen Belt is primarily an organic part of the accretionary wedge of the Outer Western Carpathians and it is overthrusted onto the Flysch Belt. This was followed by modification of the structures, mostly in a transpressional regime, including local reversing overthrusts and the development of a steep fault boundary, mainly along the southern margin, against the Inner Carpathian Paleogene succession. These differences between the structure of the western and eastern Klippen Belt segments indicate the contrast between the interaction of the western and eastern parts of the Inner Western Carpathians with the European Platform. In the western part, oblique collision and sinistral transpression dominate. In the eastern part, by contrast, subduction and orthogonal collision dominated over later transpressional modifications. LA - English DB - MTMT ER - TY - JOUR AU - Bilic, Sime AU - Garasic, Vesnica TI - Petrological characteristics of clastic sedimentary rocks from the St. Barbara ore mine in Rude near Samobor JF - RUDARSKO GEOLOSKO NAFTNI ZBORNIK - MINING GELOLOGICAL PETROLEUM ENGINEERING BULLETIN J2 - RUDARSKO GEOLOSKO NAFTNI ZBORNIK - MIN GEOL PETROL ENG BULL VL - 36 PY - 2021 IS - 1 SP - 121 EP - 135 PG - 15 SN - 0353-4529 DO - 10.17794/rgn.2021.1.10 UR - https://m2.mtmt.hu/api/publication/32279975 ID - 32279975 N1 - Export Date: 1 July 2022 Correspondence Address: Bilić, Š.; Faculty of Mining, Pierottijeva 6, Croatia; email: sime.bilic@rgn.hr AB - In the scope of this research, the petrographic and geochemical analyses of clastic sedimentary rocks from the St. Barbara, copper and iron ore mine in Rude near Samobor, have been made, aiming to classify and determine the provenance and environment of formation of clastic sedimentary rocks, as well as the influence of hydrothermal fluids on their properties. Eight samples were collected in total from different locations in the mine. Six of those samples have been studied in detail. The results showed structural and geochemical variability and uneven hydrothermal alteration intensity in the samples. Based on petrographic analyses, three rocks are classified as sublithoarenite, quartz arenite and quartz greywacke. Three of the samples are classified as ore breccia, ore sandstone, and ore silt-sandstone due to the pronounced hydrothermal alterations and ore mineralisation. Comprehensively, petrographic and geochemical analyses indicate that the source rocks of the investigated clastic sedimentary rocks were felsic (La/Sc = 0.9-6.2; Th/Sc = 1.3-2.4), most probably sedimentary, possibly resedimented rocks. The extent of source rock weathering was very high (Chemical Index of Alteration CIA = 52.1-81.3 %) and the geotectonic position of the sedimentary basin was very likely to be at the passive continental margin. LA - English DB - MTMT ER - TY - JOUR AU - Botor, Dariusz TI - Burial and Thermal History Modeling of the Paleozoic-Mesozoic Basement in the Northern Margin of the Western Outer Carpathians (Case Study from Pilzno-40 Well, Southern Poland) JF - MINERALS J2 - MINERALS-BASEL VL - 11 PY - 2021 IS - 7 PG - 23 SN - 2075-163X DO - 10.3390/min11070733 UR - https://m2.mtmt.hu/api/publication/32348229 ID - 32348229 N1 - Cited By :1 Export Date: 1 July 2022 Correspondence Address: Botor, D.; Faculty of Geology, Poland; email: botor@agh.edu.pl AB - Hydrocarbon exploration under thrust belts is a challenging frontier globally. In this work, 1-D thermal maturity modeling of the Paleozoic-Mesozoic basement in the northern margin of the Western Outer Carpathians was carried out to better explain the thermal history of source rocks that influenced hydrocarbon generation. The combination of Variscan burial and post-Variscan heating due to elevated heat flow may have caused significant heating in the Paleozoic basement in the pre-Middle Jurassic period. However, the most likely combined effect of Permian-Triassic burial and Late Triassic-Early Jurassic increase of heat flow caused the reaching of maximum paleotemperature. The main phase of hydrocarbon generation in Paleozoic source rocks developed in pre-Middle Jurassic times. Therefore, generated hydrocarbons from Ordovician and Silurian source rocks were lost before reservoirs and traps were formed in the Late Mesozoic. The Miocene thermal overprint due to the Carpathian overthrust probably did not significantly change the thermal maturity of organic matter in the Paleozoic-Mesozoic strata. Thus, it can be concluded that petroleum accumulations in the Late Jurassic and Cenomanian reservoirs of the foreland were charged later, mainly by source rocks occurring within the thrustbelt, i.e., Oligocene Menilite Shales. Finally, this work shows that comprehensive mineralogical and geochemical studies are an indispensable prerequisite of any petroleum system modelling because their results could influence petroleum exploration of new oil and gas fields. LA - English DB - MTMT ER - TY - JOUR AU - DEREROVA, J. AU - BIELIK, M. AU - KOHUT, I. AU - GODOVA, D. AU - MOJZES, A. TI - Rheological model of the lithosphere along profile VII in the Eastern Carpathians JF - CONTRIBUTIONS TO GEOPHYSICS AND GEODESY J2 - CONTRIB GEOPHYS GEODES VL - 51 PY - 2021 IS - 3 SP - 245 EP - 263 PG - 19 SN - 1335-2806 DO - 10.31577/congeo.2021.51.3.3 UR - https://m2.mtmt.hu/api/publication/32915031 ID - 32915031 N1 - Division of Geophysics, Earth Science Institute of the Slovak Academy of Sciences, Dubravska cesta 9, Bratislava, 840 05, Slovakia Department of Engineering Geology, Hydrogeology and Applied Geophysics, Faculty of Natural Sciences, Comenius University, Mlynska dolina, Ilkovicova 6, Bratislava, 842 48, Slovakia Export Date: 1 July 2022 Correspondence Address: DEREROVA, J.; Division of Geophysics, Dubravska cesta 9, Slovakia; email: geofjade@savba.sk LA - English DB - MTMT ER - TY - JOUR AU - Di Capua, A. AU - Barilaro, F. AU - Szepesi, János AU - Haranginé Lukács, Réka AU - Gál, Péter AU - Norini, G. AU - Sulpizio, R. AU - Soós, Ildikó AU - Harangi, Szabolcs AU - Groppelli, G. TI - Correlating volcanic dynamics and the construction of a submarine volcanogenic apron: An example from the Badenian (Middle Miocene) of North-Eastern Hungary JF - MARINE AND PETROLEUM GEOLOGY J2 - MAR PETROL GEOL VL - 126 PY - 2021 SN - 0264-8172 DO - 10.1016/j.marpetgeo.2021.104944 UR - https://m2.mtmt.hu/api/publication/31846118 ID - 31846118 N1 - CNR IGAG – Institute of Environmental Geology and Geoengineering, Via M. Bianco 9, Milan, 20131, Italy University of Insubria, Department of Science and High Technology, Via Valleggio 11, Como, Italy MTA – ELTE Volcanology Research Group, Budapest, Hungary Isotope Climatology and Environmental Research Centre (ICER), Institute for Nuclear Research, Hungarian Academy of Debrecen, Debrecen, Hungary University of Bari “Aldo Moro”, Department of Earth and Geoenvironmental Sciences, Via Orabona 4, Bari, 70125, Italy Eötvös Loránd University, Department of Petrology and Geochemistry, Budapest, Hungary Export Date: 8 February 2021 Correspondence Address: Di Capua, A.; CNR IGAG – Institute of Environmental Geology and Geoengineering, Via M. Bianco 9, Italy; email: andrea.dicapua@igag.cnr.it CNR IGAG – Institute of Environmental Geology and Geoengineering, Via M. Bianco 9, Milan, 20131, Italy University of Insubria, Department of Science and High Technology, Via Valleggio 11, Como, Italy MTA – ELTE Volcanology Research Group, Budapest, Hungary Isotope Climatology and Environmental Research Centre (ICER), Institute for Nuclear Research, Hungarian Academy of Debrecen, Debrecen, Hungary University of Bari “Aldo Moro”, Department of Earth and Geoenvironmental Sciences, Via Orabona 4, Bari, 70125, Italy Eötvös Loránd University, Department of Petrology and Geochemistry, Budapest, Hungary Export Date: 9 March 2021 Correspondence Address: Di Capua, A.; CNR IGAG – Institute of Environmental Geology and Geoengineering, Via M. Bianco 9, Italy; email: andrea.dicapua@igag.cnr.it CNR IGAG – Institute of Environmental Geology and Geoengineering, Via M. Bianco 9, Milan, 20131, Italy University of Insubria, Department of Science and High Technology, Via Valleggio 11, Como, Italy MTA – ELTE Volcanology Research Group, Budapest, Hungary Isotope Climatology and Environmental Research Centre (ICER), Institute for Nuclear Research, Hungarian Academy of Debrecen, Debrecen, Hungary University of Bari “Aldo Moro”, Department of Earth and Geoenvironmental Sciences, Via Orabona 4, Bari, 70125, Italy Eötvös Loránd University, Department of Petrology and Geochemistry, Budapest, Hungary Export Date: 10 March 2021 Correspondence Address: Di Capua, A.; CNR IGAG – Institute of Environmental Geology and Geoengineering, Via M. Bianco 9, Italy; email: andrea.dicapua@igag.cnr.it CNR IGAG – Institute of Environmental Geology and Geoengineering, Via M. Bianco 9, Milan, 20131, Italy University of Insubria, Department of Science and High Technology, Via Valleggio 11, Como, Italy MTA – ELTE Volcanology Research Group, Budapest, Hungary Isotope Climatology and Environmental Research Centre (ICER), Institute for Nuclear Research, Hungarian Academy of Debrecen, Debrecen, Hungary University of Bari “Aldo Moro”, Department of Earth and Geoenvironmental Sciences, Via Orabona 4, Bari, 70125, Italy Eötvös Loránd University, Department of Petrology and Geochemistry, Budapest, Hungary Export Date: 28 May 2021 Correspondence Address: Di Capua, A.; CNR IGAG – Institute of Environmental Geology and Geoengineering, Via M. Bianco 9, Italy; email: andrea.dicapua@igag.cnr.it LA - English DB - MTMT ER - TY - JOUR AU - Erdős, Zoltán AU - Huismans, Ritske S. AU - Faccenna, Claudio AU - Wolf, Sebastian G. TI - The role of subduction interface and upper plate strength on back‐arc extension: application to Mediterranean back‐arc basins JF - TECTONICS J2 - TECTONICS VL - 40 PY - 2021 IS - 8 SN - 0278-7407 DO - 10.1029/2021TC006795 UR - https://m2.mtmt.hu/api/publication/32112689 ID - 32112689 N1 - Institute of Earth Physics and Space Science, Eötvös Loránd Research Network, Sopron, Hungary Department of Geophysics and Space Science, Eötvös Loránd University, Budapest, Hungary Department of Earth Sciences, University of Bergen, Bergen, Norway Department of Science, University Roma Tre, Roma, Italy Jackson School of Geoscience, University of Texas at Austin, Austin, TX, United States Cited By :1 Export Date: 14 February 2022 Correspondence Address: Erdős, Z.; Institute of Earth Physics and Space Science, Hungary; email: zoltan-erdos@staff.elte.hu LA - English DB - MTMT ER - TY - JOUR AU - Fodor, László AU - Balázs, Attila AU - Csillag, Gábor AU - Dunkl, István AU - Héja, Gábor AU - Jelen, B AU - Kelemen, Péter AU - Kövér, Szilvia AU - Németh, A AU - Nyíri, D AU - Selmeczi, Ildikó AU - Trajanova, M AU - Vrabec, M AU - Vrabec, M TI - Crustal exhumation and depocenter migration from the Alpine orogenic margin towards the Pannonian extensional back-arc basin controlled by inheritance JF - GLOBAL AND PLANETARY CHANGE J2 - GLOBAL PLANET CHANGE VL - 201 PY - 2021 PG - 31 SN - 0921-8181 DO - 10.1016/j.gloplacha.2021.103475 UR - https://m2.mtmt.hu/api/publication/31936855 ID - 31936855 N1 - Department of Geology, Eötvös University, Pázmány Péter sétány 1/C, Budapest, 1117, Hungary ELKH-ELTE Geological, Geophysical and Space Science Research Group at Eötvös University, Hungary ETH Zürich, Geophysical Fluid Dynamics Group, Institute of Geophysics, Zürich, Switzerland Research Centre for Astronomy and Earth Sciences, Institute for Geological and Geochemical Research, Budaörsi út 45, Budapest, 1112, Hungary Sedimentology, Environmental Geology, Geoscience Center, University of Göttingen, Goldschmidtstrasse 3, Göttingen, D-37077, Germany Mining and Geological Survey of Hungary, Stefánia út 14, Budapest, 1143, Hungary Geological Survey of Slovenia, Dimičeva 14, Ljubljana, Slovenia Department of Petrology and Geochemistry, Eötvös University, Budapest, Hungary MOL Plc., Október 23. u. 18, Budapest, 1117, Hungary Department of Geology, University of Ljubljana, Faculty of Natural Sciences and Engineering, Aškerčeva 12, Ljubljana, 1000, Slovenia Cited By :7 Export Date: 1 July 2022 CODEN: GPCHE Correspondence Address: Fodor, L.; Department of Geology, Hungary; email: imre.laszlo.fodor@ttk.elte.hu LA - English DB - MTMT ER - TY - JOUR AU - Hencz, Mátyás AU - Biró, Tamás AU - Cseri, Zoltán AU - Karátson, Dávid AU - Márton Péterné Szalay, Emőke AU - Németh, Károly AU - Szakács, Alexandru AU - Pécskay, Zoltán AU - Kovács, István János TI - A Lower Miocene pyroclastic-fall deposit from the Bukk Foreland Volcanic Area, Northern Hungary: Clues for an eastward-located source JF - GEOLOGICA CARPATHICA J2 - GEOL CARPATH VL - 72 PY - 2021 IS - 1 SP - 26 EP - 47 PG - 22 SN - 1335-0552 DO - 10.31577/GeolCarp.72.1.3 UR - https://m2.mtmt.hu/api/publication/31929072 ID - 31929072 N1 - Funding Agency and Grant Number: Hungarian Scientific Research FundOrszagos Tudomanyos Kutatasi Alapprogramok (OTKA) [K115472, K128122, K128625, K131894]; New National Excellence - Program of the Ministry of Innovation and Technology from the source of the National Research, Development and Innovation Found [UNKP-20-4, UNKP-20-4-II-ELTE-32]; European UnionEuropean Commission; State of Hungary; European Regional Development FundEuropean Commission [GINOP-2.3.2.-15-2016-00009] Funding text: This work was supported by the Hungarian Scientific Research Fund projects no. K115472, K128122, K128625 and K131894. Volcanological research of T.B. was supported by the UNKP-20-4 New National Excellence - Program of the Ministry of Innovation and Technology from the source of the National Research, Development and Innovation Found (UNKP-20-4-II-ELTE-32). The research was supported by the European Union and the State of Hungary, co-financed by the European Regional Development Fund in the project GINOP-2.3.2.-15-2016-00009 `ICER`. We want to thank editor Lukas Krmicek for handling of the manuscript, and Christoph Breitkreuz and Prokop Zavada reviewers for the constructive and helpful comments. AB - Detailed investigation of a Lower Miocene Plinian pyroclastic sequence that crops out in the Bukk Foreland Volcanic Area (BFVA) in Northern Hungary is presented here. The studied eruptive products are part of a ca. 50 metres thick pyroclastic succession comprising of a basal ignimbrite that is covered by stratified pyroclastic unit including a topmost ignimbrite (Mango ignimbrite unit, part of the Lower Pyroclastic Complex). The investigated pyroclastic unit is part of the Mango ignimbrite unit, and consists of a pyroclastic fallout deposit, a ground-surge deposit, and an ignimbrite, all indicating a complete Plinian eruption phase. This pyroclastic succession has been identified in three locations, which crops out along a similar to 20 km long, SW-NE transect in the BFVA (two in the western, and one in the eastern part). The pyroclastic rocks in these sites are correlated well on the basis of the lithologically and texturally similar layers and their identical field volcanological properties. The correlation is also supported by the paleomagnetic signature of the two ignimbrites (upper ignimbrite - declination: 275-302 degrees, lower ignimbrite with overprint magnetization - declination: 320-334 degrees). The paleomagnetic directions of the stratigraphically upper ignimbrite suggest that this sequence belongs to the oldest known pyroclastic rock assemblages of the BFVA (Lower Pyroclastic Complex, deposited between 18.5 and 21 Ma according to previously published K/Ar dating results in good agreement with paleomagnetic measurements). Based on proximal-to-distal variations in the grain size of the pyroclastic fallout deposit (with maximal thickness is 71 cm), a potential source region to the east (or northeast, or southeast) of the BFVA has been inferred in a relatively close distance (similar to 5-15 km). The (north)eastward-located source region is also supported by comparison of the characteristics of the studied fallout deposit with the spatial distribution of selected Plinian fallout tephra from worldwide examples using their digitalized isopach maps. LA - English DB - MTMT ER - TY - JOUR AU - Hencz, Mátyás AU - Biró, Tamás AU - Kovács, István János AU - Stalder, R. AU - Németh, Károly AU - Szakács, Alexandru AU - Pálos, Zsófia AU - Pécskay, Zoltán AU - Karátson, Dávid TI - Uniform “water” content in quartz phenocrysts from silicic pyroclastic fallout deposits – implications on pre-eruptive conditions JF - EUROPEAN JOURNAL OF MINERALOGY J2 - EUR J MINERAL VL - 33 PY - 2021 IS - 5 SP - 571 EP - 589 PG - 19 SN - 0935-1221 DO - 10.5194/ejm-33-571-2021 UR - https://m2.mtmt.hu/api/publication/32239855 ID - 32239855 LA - English DB - MTMT ER - TY - JOUR AU - Jacko, S. AU - Jacko sen, S. AU - Labant, S. AU - Bátorová, K. AU - Farkašovský, R. AU - Ščerbáková, B. TI - Structural contraints of neotectonic activity in the eastern part of the western carpathians orogenic wedge JF - QUATERNARY INTERNATIONAL J2 - QUATERN INT VL - 585 PY - 2021 SP - 27 EP - 43 PG - 17 SN - 1040-6182 DO - 10.1016/j.quaint.2020.10.072 UR - https://m2.mtmt.hu/api/publication/31655214 ID - 31655214 N1 - Institute of Geo-sciences, Faculty BERG, Technical University of Košice04001, Slovakia Institute of Geodesy, Cartography and GIS, Faculty BERG, Technical University of Košice, Kosice, 04001, Slovakia Cited By :4 Export Date: 14 February 2022 Correspondence Address: Jacko, S.; Institute of Geo-sciences, Slovakia; email: stanislav.jacko@tuke.sk LA - English DB - MTMT ER - TY - JOUR AU - Kondor, Henrietta AU - M. Tóth, Tivadar TI - Contrasting metamorphic and post-metamorphic evolutions within the Algyő basement high (Tisza Mega-unit, SE Hungary). Consequences for structural history JF - CENTRAL EUROPEAN GEOLOGY J2 - CENT EUR GEOL VL - 64 PY - 2021 IS - 2 SP - 91 EP - 112 PG - 22 SN - 1788-2281 DO - 10.1556/24.2021.00004 UR - https://m2.mtmt.hu/api/publication/32055044 ID - 32055044 N1 - Export Date: 12 September 2021 Correspondence Address: KONDOR, H.; Department of Mineralogy Geochemistry and Petrology, Egyetem st. 2, Hungary; email: kondor.henrietta@gmail.com LA - English DB - MTMT ER - TY - JOUR AU - Kovacs, M AU - Fülöp, A AU - Seghedi, I AU - Pécskay, Zoltán TI - Architecture of volcanic plumbing systems inferred from thermobarometry: A case study from the Miocene Gutâi Volcanic Zone in the Eastern Carpathians, Romania JF - LITHOS J2 - LITHOS VL - 396-397 PY - 2021 SN - 0024-4937 DO - 10.1016/j.lithos.2021.106191 UR - https://m2.mtmt.hu/api/publication/32016325 ID - 32016325 N1 - Tech. Univ. Cluj-Napoca, North Univ. Centre Baia Mare, Baia Mare, Romania Institute of Geodynamics Sabba S. Ştefănescu, Romanian Academy, Bucharest, Romania Institute of Nuclear Research of the Hungarian Academy of Sciences, Debrecen, Hungary Export Date: 28 May 2021 Correspondence Address: Kovacs, M.; Tech. Univ. Cluj-Napoca, Romania; email: marinel.kovacs@cunbm.utcluj.ro LA - English DB - MTMT ER - TY - JOUR AU - Leskó, Máté Zsigmond AU - Papp, Richárd Zoltán AU - Kristály, Ferenc AU - Pálfy, József AU - Zajzon, Norbert TI - Occurrence and significance of smectite in the Pliensbachian (Lower Jurassic) at Lókút 2 (Bakony Mts., Hungary) JF - CENTRAL EUROPEAN GEOLOGY J2 - CENT EUR GEOL VL - 64 PY - 2021 IS - 1 SP - 8 EP - 17 PG - 9 SN - 1788-2281 DO - 10.1556/24.2021.00002 UR - https://m2.mtmt.hu/api/publication/31711317 ID - 31711317 N1 - Institute of Mineralogy and Geology, University of Miskolc, Miskolc, Hungary Department of Geology, Eotvos Lorand University, Budapest, Hungary Research Group for Paleontology, Hungarian Academy of Sciences-Hungarian Natural History, Museum-Eotvos Lorand University, Budapest, Hungary Export Date: 30 June 2022 Correspondence Address: LESKÓ, M.Z.; Institute of Mineralogy and Geology, Hungary; email: askmate@uni-miskolc.hu A cikkben/előadásban/tanulmányban ismertetett kutató munka az EFOP-3.6.1-16-00011 jelű „Fiatalodó és Megújuló Egyetem – Innovatív Tudásváros – a Miskolci Egyetem intelligens szakosodást szolgáló intézményi fejlesztése” projekt részeként – a Széchenyi 2020 keretében – az Európai Unió támogatásával, az Európai Szociális Alap társfinanszírozásával valósul meg = “The described article/presentation/study was carried out as part of the EFOP-3.6.1-16-00011 “Younger and Renewing University – Innovative Knowledge City – institutional development of the University of Miskolc aiming at intelligent specialisation” project implemented in the framework of the Szechenyi 2020 program. The realization of this project is supported by the European Union, co-financed by the European Social Fund.” LA - English DB - MTMT ER - TY - JOUR AU - Liptai, Nóra AU - Berkesi, Márta AU - Patkó, Levente AU - Bodnár, RJ AU - O’Reilly, SY AU - Griffin, WL AU - Szabó, Csaba TI - Characterization of the metasomatizing agent in the upper mantle beneath the northern Pannonian Basin based on Raman imaging, FIB-SEM and LA-ICP-MS analyses of silicate melt inclusions in spinel peridotite JF - AMERICAN MINERALOGIST J2 - AM MINERAL VL - 106 PY - 2021 IS - 5 SP - 685 EP - 700 PG - 16 SN - 0003-004X DO - 10.2138/am-2021-7292 UR - https://m2.mtmt.hu/api/publication/31956559 ID - 31956559 N1 - Lithosphere Fluid Research Lab, Institute of Geography and Earth Sciences, Eötvös University, 1/C Pázmány Péter sétány, Budapest, H-1117, Hungary Australian Research Council Centre of Excellence for Core to Crust Fluid Systems (CCFS) and Gemoc, Department of Earth and Planetary Sciences, Macquarie University, Herring Road, North Ryde, NSW 2019, Australia Institute for Nuclear Research, Isotope Climatology and Environmental Research Centre, 18/C Bem tér, Debrecen, Hungary Fluids Research Laboratory, Department of Geosciences, Virginia Tech, 926 West Campus Drive, Blacksburg, VA, United States Geodetic and Geophysical Institute, Research Centre for Astronomy and Earth Sciences, 6-8 Csatkai Endre u, Sopron, 9400, Hungary Cited By :2 Export Date: 1 July 2022 Correspondence Address: Liptai, N.; Lithosphere Fluid Research Lab, 1/C Pázmány Péter sétány, Hungary; email: n.liptai.elte@gmail.com LA - English DB - MTMT ER - TY - JOUR AU - Liptai, Nóra AU - Lange, Thomas Pieter AU - Patkó, Levente AU - Pintér, Zsanett AU - Berkesi, Márta AU - Aradi, László Előd AU - Szabó, Csaba AU - Kovács, István János TI - Effect of water on the rheology of the lithospheric mantle in young extensional basin systems as shown by xenoliths from the Carpathian-Pannonian region JF - GLOBAL AND PLANETARY CHANGE J2 - GLOBAL PLANET CHANGE VL - 196 PY - 2021 PG - 12 SN - 0921-8181 DO - 10.1016/j.gloplacha.2020.103364 UR - https://m2.mtmt.hu/api/publication/31655281 ID - 31655281 N1 - MTA CSFK Lendület Pannon LitH2Oscope Research Group, Geodetic and Geophysical Institute, Research Centre for Astronomy and Earth Sciences, Sopron, Hungary Geodetic and Geophysical Institute, Research Centre for Astronomy and Earth Sciences, Sopron, Hungary Lithosphere Fluid Research Lab, Institute of Geography and Earth Sciences, Eötvös Loránd University, Budapest, Hungary Isotope Climatology and Environmental Research Centre, Institute for Nuclear Research, Debrecen, Hungary School of Earth, Atmosphere and Environment, Monash University, Melbourne, Australia Export Date: 27 November 2020 CODEN: GPCHE Correspondence Address: Liptai, N.; MTA CSFK Lendület Pannon LitH2Oscope Research Group, Mining and Geological Survey of HungaryHungary; email: liptai.nora@csfk.mta.hu Funding Agency and Grant Number: Lendulet Research Grant; ELTE Institutional Excellence Program by the Hungarian Ministry of Human Capacities [1783-3/2018/FEKUTSRAT]; Hungarian Scientific Research FundOrszagos Tudomanyos Kutatasi Alapprogramok (OTKA) [NN128629]; [GINOP2.3.2-15-2016-00009] Funding text: The authors owe thanks to Judith Mihaly and Csaba Nemeth for their help with FTIR analyses. We are grateful for the detailed and constructive reviews of Wolfram Geissler and Ioan Seghedi, as well as for the editorial handling by Liviu Matenco. This study was financially supported by a Lendulet Research Grant to the MTA CSFK Lendulet Pannon LitH2Oscope Research Group, the ELTE Institutional Excellence Program (1783-3/2018/FEKUTSRAT) by the Hungarian Ministry of Human Capacities to L. Patko, L. E. Aradi, M. Berkesi and Cs. Szabo, the GINOP2.3.2-15-2016-00009 research program to L. Patko, and the Hungarian Scientific Research Fund (grant nr. NN128629, Topo-Transylvania) to I. Kovacs. The manuscript is dedicated to the memory of Prof. Frank Horvath, who was a pioneer in building cooperations between geophysical and geochemical research. MTA CSFK Lendület Pannon LitH2Oscope Research Group, Geodetic and Geophysical Institute, Research Centre for Astronomy and Earth Sciences, Sopron, Hungary Geodetic and Geophysical Institute, Research Centre for Astronomy and Earth Sciences, Sopron, Hungary Lithosphere Fluid Research Lab, Institute of Geography and Earth Sciences, Eötvös Loránd University, Budapest, Hungary Isotope Climatology and Environmental Research Centre, Institute for Nuclear Research, Debrecen, Hungary School of Earth, Atmosphere and Environment, Monash University, Melbourne, Australia Cited By :1 Export Date: 16 February 2021 CODEN: GPCHE Correspondence Address: Liptai, N.; MTA CSFK Lendület Pannon LitH2Oscope Research Group, Hungary; email: liptai.nora@csfk.mta.hu Funding details: GINOP-2.3.2-15-2016-00009 Funding details: Hungarian Scientific Research Fund, OTKA Funding text 1: The authors owe thanks to Judith Mihály and Csaba Németh for their help with FTIR analyses. We are grateful for the detailed and constructive reviews of Wolfram Geissler and Ioan Seghedi, as well as for the editorial handling by Liviu Matenco. This study was financially supported by a Lendület Research Grant to the MTA CSFK Lendület Pannon LitH 2 Oscope Research Group, the ELTE Institutional Excellence Program (1783-3/2018/FEKUTSRAT) by the Hungarian Ministry of Human Capacities to L. Patkó, L. E. Aradi, M. Berkesi and Cs. Szabó, the GINOP-2.3.2-15-2016-00009 research program to L. Patkó, and the Hungarian Scientific Research Fund (grant nr. NN128629, Topo-Transylvania) to I. Kovács. The manuscript is dedicated to the memory of Prof. Frank Horváth, who was a pioneer in building cooperations between geophysical and geochemical research. MTA CSFK Lendület Pannon LitH2Oscope Research Group, Geodetic and Geophysical Institute, Research Centre for Astronomy and Earth Sciences, Sopron, Hungary Geodetic and Geophysical Institute, Research Centre for Astronomy and Earth Sciences, Sopron, Hungary Lithosphere Fluid Research Lab, Institute of Geography and Earth Sciences, Eötvös Loránd University, Budapest, Hungary Isotope Climatology and Environmental Research Centre, Institute for Nuclear Research, Debrecen, Hungary School of Earth, Atmosphere and Environment, Monash University, Melbourne, Australia Export Date: 28 May 2021 CODEN: GPCHE Correspondence Address: Liptai, N.; MTA CSFK Lendület Pannon LitH2Oscope Research Group, Hungary; email: liptai.nora@csfk.mta.hu LA - English DB - MTMT ER - TY - JOUR AU - Hargitainé Molnár, Zsuzsa AU - Baloghné Kiss, Gabriella AU - Molnár, Ferenc AU - Váczi, Tamás AU - Czuppon, György AU - Dunkl, István AU - Zaccarini, F. AU - Dódony, István TI - Epigenetic-hydrothermal fluorite veins in a phosphorite deposit from balaton highland (Pannonian basin, Hungary): Signatures of a regional fluid flow system in an alpine triassic platform JF - MINERALS J2 - MINERALS-BASEL VL - 11 PY - 2021 IS - 6 PG - 19 SN - 2075-163X DO - 10.3390/min11060640 UR - https://m2.mtmt.hu/api/publication/32078777 ID - 32078777 N1 - Department of Mineralogy, Eötvös Loránd University, Pázmány P. Street 1/C, Budapest, H‐1117, Hungary Geological Survey of Finland, Vuorimiehentie 5, P.O. Box 96, Espoo, FI‐02151, Finland Wigner Research Centre for Physics, Eötvös Loránd Research Network, Konkoly‐Thege Miklós Street 29–33, Budapest, H‐1124, Hungary Research Centre for Astronomy and Earth Sciences, Institute for Geological and Geochemical Research, Eötvös Loránd Research Network, Budaörsi Street 45, Budapest, H‐1112, Hungary Geoscience Center, Department of Sedimentology and Environmental Geology, University of Göttingen, Goldschmidtstrasse 3, Göttingen, D‐37077, Germany Department of Applied Geosciences and Geophysics, University of Leoben, Peter Tunner Street 5, Leoben, A‐8700, Austria Cited By :2 Export Date: 25 March 2024 Correspondence Address: Molnár, Z.; Department of Mineralogy, Pázmány P. Street 1/C, Hungary; email: molnarzsuzsa89@gmail.com Correspondence Address: Kiss, G.B.; Department of Mineralogy, Pázmány P. Street 1/C, Hungary; email: gabriella.b.kiss@ttk.elte.hu LA - English DB - MTMT ER - TY - JOUR AU - Nagy, Zsolt AU - Baracza, Mátyás Krisztián AU - Szabó, Norbert Péter TI - Magnitude Estimation of Overpressure Generation Mechanisms Using Quantitative Stochastic 2D Basin Models: A Case Study from the Danube-Tisza Interfluve Area in Hungary JF - APPLIED SCIENCES-BASEL J2 - APPL SCI-BASEL VL - 11 PY - 2021 IS - 6 PG - 25 SN - 2076-3417 DO - 10.3390/app11062841 UR - https://m2.mtmt.hu/api/publication/31930222 ID - 31930222 N1 - Export Date: 2 December 2022 LA - English DB - MTMT ER - TY - JOUR AU - Németh, Bianka AU - Török, Kálmán AU - Bali, E AU - Zajacz, Z AU - Fodor, László AU - Szabó, Csaba TI - Melt-rock interaction in the lower crust based on silicate melt inclusions in mafic garnet granulite xenoliths, Bakony-Balaton Highland Volcanic Field (Hungary) JF - GEOLOGICA CARPATHICA J2 - GEOL CARPATH VL - 72 PY - 2021 IS - 3 SP - 232 EP - 252 PG - 21 SN - 1335-0552 DO - 10.31577/GeolCarp.72.3.4 UR - https://m2.mtmt.hu/api/publication/32116865 ID - 32116865 N1 - Mining and Geological Survey of Hungary, Stefánia Road 14., Budapest, H-1143, Hungary MTA-ELTE Volcanology Research Group, Eötvös University, Pázmány Péter sétány 1/c, Budapest, H-1117, Hungary Lithosphere Fluid Research Lab (LRG), Department of Petrology and Geochemistry, Eötvös Loránd University, Pázmány Péter sétány 1/c, Budapest, H-1117, Hungary Nordic Volcanological Institute, Institute of Earth Sciences, University of Iceland, Sturlugata 7, Reykjavík, 101, Iceland Department of Earth Sciences, Institute of Isotope Geochemistry and Mineral Resources, ETH Zürich, Zürich, 8092, Switzerland Section of Earth and Environmental Sciences, University of Geneva, Switzerland Department of Geology, Eötvös Loránd University, Pázmány Péter sétány 1/c, Budapest, H-1117, Hungary MTA-ELTE Geological, Geophysical and Space Science Research Group, Eötvös University, Pázmány Péter sétány 1/c, Budapest, H-1117, Hungary Export Date: 30 June 2022 Correspondence Address: Németh, B.; Mining and Geological Survey of Hungary, Stefánia Road 14., Hungary; email: nemethbj@student.elte.hu AB - Major and trace element composition of silicate melt inclusions (SMI) and their rock-forming minerals were studied in mafic garnet granulite xenoliths from the Bakony-Balaton Highland Volcanic Field (Western Hungary). Primary SMIs occur in clinopyroxene and plagioclase in the plagioclase-rich domains of mafic garnet granulites and in ilmenite in the vicinity of these domains in the wall rock. Based on major and trace elements, we demonstrated that the SMIs have no connection with the xenolith-hosting alkaline basalt as they have rhyodacitic composition with a distinct REE pattern, negative Sr anomaly, and HFSE depletion. The trace element characteristics suggest that the clinopyroxene hosted SMIs are the closest representation of the original melt percolated in the lower crust. In contrast, the plagioclase and ilmenite hosted SMIs arc products of interaction between the silicic melt and the wall rock garnet granulite. A further product of this interaction is the clinopyroxene-ilmeniteiplagioclase symplectite. Textural observations and mass balance calculations reveal that the reaction between titanite and the silicate melt led to the formation of these assemblages. We propose that a tectonic melange of metapelites and (MOR-related) metabasalts partially melted at 0.3-0.5 GPa to form a dacitic-rhyodacitic melt leaving behind a garnet-free, plagioclaseclinopyroxene+orthopyroxene+ilmenite residuum. The composition of the SMIs (both major and trace elements) is similar to those from the middle Miocene calc-alkaline magmas, widely known from the northern Pannonian Basin (BOrzsOny and Visegrad Mts., Cserhat and Matra volcanic areas and Central Slovakian VF), but the SMIs are probably the result of a later, local process. The study of these SMIs also highlights how crustal contamination changes magma compositions during asthenospheric Miocene ascent. LA - English DB - MTMT ER - TY - JOUR AU - Obbágy, Gabriella AU - Dunkl, István AU - Józsa, Sándor AU - Silye, Lóránd AU - Arató, Róbert AU - Lünsdorf, NK AU - von Eynatten, H TI - Paleogeographic implications of a multi-parameter Paleogene provenance dataset (Transylvanian Basin, Romania) JF - JOURNAL OF SEDIMENTARY RESEARCH J2 - J SEDIMENT RES VL - 91 PY - 2021 IS - 6 SP - 551 EP - 570 PG - 20 SN - 1527-1404 DO - 10.2110/jsr.2020.080 UR - https://m2.mtmt.hu/api/publication/32075619 ID - 32075619 N1 - Department of Petrology and Geochemistry, Eötvös Loránd University, Pázmány Péter sétány 1/C, Budapest, H-1117, Hungary Geoscience Center, Department of Sedimentology and Environmental Geology, University of Göttingen, Goldschmidtstrasse 3, Göttingen, D-37077, Germany Isotope Climatology and Environmental Research Centre, Institute for Nuclear Research, Hungarian Academy of Sciences, Bem tér 18/C, Debrecen, H-4026, Hungary Department of Geology, Babeş-Bolyai University, M. Kogalniceanu street 1, Cluj-Napoca, RO-400084, Romania Export Date: 23 September 2021 Correspondence Address: Obbágy, G.; Department of Petrology and Geochemistry, Pázmány Péter sétány 1/C, Hungary; email: obbagy.gabriella@atomki.mta.hu LA - English DB - MTMT ER - TY - JOUR AU - Šujan, M AU - Rybár, S AU - Kováč, M AU - Bielik, M AU - Majcin, D AU - Minár, J AU - Plašienka, D AU - Nováková, P AU - Kotulová, J TI - The polyphase rifting and inversion of the Danube Basin revised JF - GLOBAL AND PLANETARY CHANGE J2 - GLOBAL PLANET CHANGE VL - 196 PY - 2021 SN - 0921-8181 DO - 10.1016/j.gloplacha.2020.103375 UR - https://m2.mtmt.hu/api/publication/31659943 ID - 31659943 N1 - Funding Agency and Grant Number: Slovak Research and Development Agency (APVV)Slovak Research and Development Agency [APVV-15-0575, APVV-16-0121, APVV-16-0146, APVV-16-0482, APVV-17-0170, APVV-19-0150]; Scientific Grant Agency of the Ministry of Education, Science, Research and Sport of the Slovak Republic [2/0006/19]; Slovak Academy of Sciences (VEGA)Vedecka grantova agentura MSVVaS SR a SAV (VEGA) [2/0006/19] Funding text: This study is dedicated to the memory of Frank Horvath, whose strong motivation and innovative ideas in research of the Pannonian Basin will be deeply missed in the scientific community. The individual authors of the study were supported financially by the Slovak Research and Development Agency (APVV) under contracts Nos. APVV-15-0575, APVV-16-0121, APVV-16-0146, APVV-16-0482, APVV-17-0170 and APVV-19-0150 and by the Scientific Grant Agency of the Ministry of Education, Science, Research and Sport of the Slovak Republic and the Slovak Academy of Sciences (VEGA) under the contract No. 2/0006/19. Schlumberger ltd. is acknowledged for providing academic license of the PetroMod software to the Faculty of Natural Sciences, Comenius University in Bratislava. We are thankfull to Attila Bartha and Teodoro Cassola (Schlumberger ltd.) for their kind help during the 1D subsidence modelling. We are particularly grateful to the associate editor Liviu Matenco and to the reviewers Gabor Tad, Eline Le Breton, ZsOfia Ruszkiczay-Rtidiger and two anonymous reviewers for precise and constructive comments, which allowed us to significantly improve the manuscript. MS is indebted to ZsOfia Ruszkiczay-Rtidiger for fruitful discussion on the evolution of the Danube Basin area during its inversion. This research highly benefited from the collaboration with Regis Braucher and his colleagues (CEREGE, Aix-en-Provence, France), which allowed us to accomplish an extensive published geochronological dataset that supported the study. The long-term cooperation with Lubomfr Sliva and Nafta, a.s, was crucial for obtaining well-cores and seismic data used in the research and is highly acknowledged. The precise language correction done by Adam TomaSovYch is highly appreciated. LA - English DB - MTMT ER - TY - JOUR AU - Szemerédi, Máté AU - Raucsikné Varga, Andrea Beáta AU - Dunkl, I. AU - Haranginé Lukács, Réka AU - Seghedi, I. AU - Kovács, Zoltán AU - Raucsik, Béla AU - Pál-Molnár, Elemér TI - Petrology and zircon U–Pb dating of granitoid rocks in the Highiş massif (SW Apuseni Mts., Romania): Insights into Permian plutonic–volcanic connections JF - GEOLOGICA CARPATHICA J2 - GEOL CARPATH VL - 72 PY - 2021 IS - 6 SP - 482 EP - 504 PG - 23 SN - 1335-0552 DO - 10.31577/GeolCarp.72.6.3 UR - https://m2.mtmt.hu/api/publication/32558406 ID - 32558406 LA - English DB - MTMT ER - TY - JOUR AU - Vitovič, L AU - Minár, J AU - Pánek, T TI - Morphotectonic configuration of the Podtatranská Kotlina Basin and its relationship to the origin of the Western Carpathians JF - GEOMORPHOLOGY J2 - GEOMORPHOLOGY VL - 394 PY - 2021 SN - 0169-555X DO - 10.1016/j.geomorph.2021.107963 UR - https://m2.mtmt.hu/api/publication/32236369 ID - 32236369 N1 - Cited By :1 Export Date: 1 July 2022 Correspondence Address: Vitovič, L.; State Geological Institute of Dionýz Štúr, Mlynská dolina 1, Slovakia; email: ladislav.vitovic@geology.sk LA - English DB - MTMT ER - TY - JOUR AU - Vozari, Jan AU - Bezak, Vladimir AU - Marko, Frantisek TI - Three-dimensional magnetotelluric model along seismic profile 2T: An improved view on crustal structure in central Slovakia (Western Carpathians) JF - GEOLOGICA CARPATHICA J2 - GEOL CARPATH VL - 72 PY - 2021 IS - 2 SP - 85 EP - 95 PG - 11 SN - 1335-0552 DO - 10.31577/GeolCarp.72.2.1 UR - https://m2.mtmt.hu/api/publication/32318191 ID - 32318191 N1 - Earth Science Institute, Division of Geophysics, Slovak Academy of Sciences, Dúbravská cesta 9, Bratislava, 840 05, Slovakia Comenius University in Bratislava, Faculty of Natural Sciences, Department of Geology and Paleontology, Ilkovičova 6, Bratislava, 842 15, Slovakia Cited By :1 Export Date: 1 July 2022 Correspondence Address: Vozár, J.; Earth Science Institute, Dúbravská cesta 9, Slovakia; email: geofjavo@savba.sk AB - We present the crustal-scale geophysical model based on the magnetotelluric method focused on 3-D modelling of the seismic 2T profile crossing the major Western Carpathian tectonic units in central Slovakia. The results of the 3-D modelling show substantial improvement in previous 2-D models of deep crustal structure in central Slovakia, mainly of the physically distinct tectonic segments and major geo-electrical regional structures like the zone of the Carpathian Conductivity Anomaly, which indicates the occurrence of the large-scale shear zone in the contact zone of the European platform and Inner Western Carpathians. Ifigh detail geo-electrical data in 3-D magnetotelluric (MT) cross section also allowed a better interpretation of other conductive anomalies. In the final integrated interpretation (combination of 3-D geo-electrical model, gravity data and seismic reflectors), it is shown that frontal part of the Inner Western Carpathians plate exhibits the transpressional tectonic style of the back-thnist Outer Western Carpathians (Flysch Belt) and Pieniny Klippen Belt units over the progressing Inner Western Carpathian thrust wedge. These back-thrusts form the southern branch of the accretionary structural fan a large-scale transpressional flower structure typical mainly but not only for oblique convergent regimes. The southernmost segment of the profile with high whole-crust conductivity due to a higher heat flow caused by young volcanic activity indicates partial melting in the middle and lower crust. LA - English DB - MTMT ER - TY - JOUR AU - Zielinska, Magdalena TI - Thermal Maturity of the Grajcarek Unit (Pieniny Klippen Belt): Insights for the Burial History of a Major Tectonic Boundary of the Western Carpathians JF - MINERALS J2 - MINERALS-BASEL VL - 11 PY - 2021 IS - 11 PG - 18 SN - 2075-163X DO - 10.3390/min11111245 UR - https://m2.mtmt.hu/api/publication/32602387 ID - 32602387 N1 - Export Date: 30 June 2022 Correspondence Address: Zielińska, M.; Faculty of Natural Sciences, 60 Bedzinska St., Poland; email: magdalena.zielinska@us.edu.pl AB - The Grajcarek Unit of the Pieniny Klippen Belt (PKB), at the boundary between the Central (Inner) and Outer Carpathians, resulted from the convergence of the ALCAPA (the Alps-Carpathians-Pannonia) block and European plate. The strongly deformed slices of the Grajcarek Unit consist of Jurassic-Cretaceous sedimentary rocks associated with Late Cretaceous-Middle Palaeocene synorogenic wild-flysch, and sedimentary breccias with olistoliths. Maximum burial temperatures and burial depths were estimated based on vitrinite reflectance data. The vitrinite reflectance values were wide scattered through the Grajcarek sedimentary succession, especially in the flysch formations. This is attributed mainly to the depositional effects that affected the vitrinite evolution. The determined maximum burial temperatures were interpreted due to the regional compression controlled by tectonic burial coeval with thrusting and strike-slip faulting. The regional vitrinite reflectance variations might estimate cumulative displacement around the NNW-SSE and oriented the strike-slip Dunajec fault, which is a continuation of the deep fracture Krakow-Myszkow fault zone. LA - English DB - MTMT ER - TY - JOUR AU - Bezak, Vladimir AU - Pek, Josef AU - Vozar, Jan AU - Majcin, Dusan AU - Bielik, Miroslav AU - Tomek, Cestmir TI - Geoelectrically distinct zones in the crust of the Western Carpathians: A consequence of Neogene strike-slip tectonics JF - GEOLOGICA CARPATHICA J2 - GEOL CARPATH VL - 71 PY - 2020 IS - 1 SP - 14 EP - + PG - 12 SN - 1335-0552 DO - 10.31577/GeolCarp.71.1.2 UR - https://m2.mtmt.hu/api/publication/31437022 ID - 31437022 N1 - Earth Science Institute of the Slovak Academy of Sciences, Dúbravská cesta 9, Bratislava, 840 05, Slovakia Institute of Geophysics, Academy of Sciences of the Czech Republic, Boční II/1401, Praha 4, 141 31, Czech Republic Department of Applied and Environmental Geophysics, Faculty of Natural Sciences, Comenius University, Mlynská dolina, Bratislava, 842 48, Slovakia Cited By :5 Export Date: 1 July 2022 Correspondence Address: Bezák, V.; Earth Science Institute of the Slovak Academy of Sciences, Dúbravská cesta 9, Slovakia; email: geofbezv@savba.sk AB - Seismic reflection profile 2T is one of the best known geophysical profiles in the Carpathian region. It is very interesting from the geological point of view, because it cross-cuts all the basic tectonic units of the Western Carpathians. This profile was only interpreted by seismic methods and has never been modelled by the magnetotelluric method or compared with results of other geophysical methods. This missing study is the main objective of our paper and results in the new interpretation of the Western Carpathian crustal structure. The 2T profile can be divided into four main independent tectonic zones from an electrical conductivity viewpoint, and this is also supported by information from seismic, gravimetric and partly geothermic results. The first zone from the north is the segment of the Outer Western Carpathians with conductive sedimentary sequences of the Flysch belt overriding the non-conductive European platform. The following zone is represented by resistive migmatitic complexes of the Tatric Unit. The next zone to the south is composed from much more conductive metamorphic complexes of the Veporic Unit. The southernmost one is characterized by very conductive structures in the whole crust. The boundaries of the zones in the geophysical crosssections are manifested by subvertical Neogene (Neoalpine) strike-slip zones. The 2-D zones visible in the cross-sections and on the maps are the projections of the separate independent crustal segments. Older tectonic structures (mainly the Paleo-alpine and Hercynian overthrusts) are preserved inside these crustal segments. LA - English DB - MTMT ER - TY - JOUR AU - Biró, Tamás AU - Hencz, Mátyás AU - Németh, Károly AU - Karátson, Dávid AU - Márton Péterné Szalay, Emőke AU - Szakács, A AU - Bradák, Balázs AU - Szalai, Zoltán AU - Pécskay, Zoltán AU - Kovács, István János TI - A Miocene Phreatoplinian eruption in the North-Eastern Pannonian Basin, Hungary : the Jató Member JF - JOURNAL OF VOLCANOLOGY AND GEOTHERMAL RESEARCH J2 - J VOLCANOL GEOTH RES VL - 401 PY - 2020 SN - 0377-0273 DO - 10.1016/j.jvolgeores.2020.106973 UR - https://m2.mtmt.hu/api/publication/31355974 ID - 31355974 N1 - Funding Agency and Grant Number: New National Excellence Program of the Ministry of Human Capacities [UNKP-16-3]; National Talent Program - Young Talents of the Nation [NTP-NFTO-18-B-0130]; Hungarian Scientific Research FundOrszagos Tudomanyos Kutatasi Alapprogramok (OTKA) [K105245, K115472, K128625, K131894, K128122]; European UnionEuropean Union (EU); State of Hungary; European Regional Development FundEuropean Union (EU) [GINOP - 2.3.2 - 15 - 2016 - 00009 ICER]; Erasmus+ International Credit Mobility, - ELTE - Massey University Research Cooperation Program; Junta de Castilla y Leon, SpainJunta de Castilla y Leon [BU235P18]; European Regional Development Fund (ERD)European Union (EU) Funding text: Physical volcanological research of TB is supported by UNKP-16-3 New National Excellence Program of the Ministry of Human Capacities and the National Talent Program - Young Talents of the Nation (NTP-NFTO-18-B-0130). Thisworkwas supported by theHungarian Scientific Research Fund project nos. K105245, K115472, K128625, K131894, K128122 and by the European Union and the State of Hungary, cofinanced by the European Regional Development Fund in the project of GINOP - 2.3.2 - 15 - 2016 - 00009 ICER. KN's contribution and field work were possible by the fund available under the Erasmus+ International Credit Mobility, - ELTE - Massey University Research Cooperation Program. Balazs Bradak acknowledges the financial support of project BU235P18 (Junta de Castilla y Leon, Spain) and the European Regional Development Fund (ERD). Zoltan Cseri (Eotvos University, Department of Physical Geography) is greatly acknowledged for conducting AMS measurements, whereas Katalin Feher (Eotvos University, Department of Environmental and LandscapeGeography) for her help during sieving and density measurements. We thank Annamaria Nagy (Research Center for Astronomy and Earth Sciences, Geographical Institute) for her assistance in laser diffraction measurements. Comments and language editing by Julie Palmer are highly appreciated. Comments and suggestions from Alexa Van Eaton (U.S. Geological Survey) and Geoff Kilgour (GNS Science, New Zealand) that enriched the original version of the manuscript are greatly acknowledged. Thanks go to Jose Luis Macias for useful comments and editorial handling of the manuscript. Export Date: 10 March 2021 Correspondence Address: Biró, T.; Eötvös University, Pázmány Péter sétány 1/C, Hungary; email: birotamas@caesar.elte.hu Export Date: 28 May 2021 Correspondence Address: Biró, T.; Eötvös University, Pázmány Péter sétány 1/C, Hungary; email: birotamas@caesar.elte.hu LA - English DB - MTMT ER - TY - JOUR AU - DÉREROVÁ, J. AU - BIELIK, M. AU - KOHÚT, I. AU - GODOVÁ, D. AU - VOZÁR, J. AU - BEZÁK, V. TI - Lithospheric model along transect HT-1 across Western Carpathians and Pannonian Basin based on 2D integrated modelling JF - JOURNAL OF TAXATION: A NATIONAL JOURNAL OF CURRENT DEVELOPMENTS, ANALYSIS, AND COMMENTARY FOR TAX PROFESSIONALS J2 - J TAX VL - 50 PY - 2020 IS - 4 SP - 463 EP - 474 PG - 12 SN - 0022-4863 DO - 10.31577/congeo.2020.50.4.5 UR - https://m2.mtmt.hu/api/publication/32915033 ID - 32915033 N1 - Division of Geophysics, Earth Science Institute of the Slovak Academy of Sciences, Dubravska cesta 9, Bratislava, 840 05, Slovakia Department of Applied and Environmental Geophysics, Faculty of Natural Sciences, Comenius University, Mlynska dolina, Ilkovicova 6, Bratislava, 842 15, Slovakia Cited By :1 Export Date: 1 July 2022 Correspondence Address: DÉREROVÁ, J.; Division of Geophysics, Dubravska cesta 9, Slovakia; email: geofjade@savba.sk LA - English DB - MTMT ER - TY - JOUR AU - Dibacto, S. AU - Lahitte, P. AU - Karátson, Dávid AU - Hencz, Mátyás AU - Szakács, A. AU - Biró, Tamás AU - Kovács, István János AU - Veres, D. TI - Growth and erosion rates of the East Carpathians volcanoes constrained by numerical models: Tectonic and climatic implications JF - GEOMORPHOLOGY J2 - GEOMORPHOLOGY VL - 368 PY - 2020 PG - 21 SN - 0169-555X DO - 10.1016/j.geomorph.2020.107352 UR - https://m2.mtmt.hu/api/publication/31389781 ID - 31389781 LA - English DB - MTMT ER - TY - JOUR AU - Győri, Orsolya AU - Haas, János AU - Hips, Kinga AU - Lukoczki, Georgina AU - Budai, Tamás AU - Demény, Attila AU - Laczkó-Dobos, Emese TI - Dolomitization of shallow-water, mixed silicilastic‑carbonate sequences: The Lower Triassic ramp succession of the Transdanubian Range, Hungary JF - SEDIMENTARY GEOLOGY J2 - SEDIMENT GEOL VL - 395 PY - 2020 PG - 20 SN - 0037-0738 DO - 10.1016/j.sedgeo.2019.105549 UR - https://m2.mtmt.hu/api/publication/30899104 ID - 30899104 N1 - MTA-ELTE Geological, Geophysical and Space Science Research Group, Pázmány P. sétány 1/c, Budapest, H–1117, Hungary Department of Physical and Applied Geology, Eötvös Loránd University, Pázmány P. sétány 1/c, Budapest, H–1117, Hungary University of Kentucky, Kentucky Geological Survey, Mining and Mineral Resources Building, Lexington, KY 40506, United States Department of Geology and Meteorology, University of Pécs, 7624 Ifjúság útja 6, Pécs, Hungary Institute for Geological and Geochemical Research, Research Centre for Astronomy and Earth Sciences, Hungarian Academy of Sciences, Budaörsi street 45, Budapest, H-1112, Hungary Cited By :5 Export Date: 30 June 2022 Correspondence Address: Győri, O.; MTA-ELTE Geological, Pázmány P. sétány 1/c, Hungary; email: gyoriorsolya@caesar.elte.hu AB - The Lower Triassic succession of the Transdanubian Range in Hungary comprises limestones, dolomite, marl, sandstones and siltstones, deposited in tidal flat, lagoon and ooid shoal environments on the marginal ramp of the western Neotethys. Seven cores were chosen for petrographic and stable isotope investigations aiming to reconstruct the paragenetic sequence with special regard to the dolomitization and hydrothermal events. Five lithotypes were differentiated: (i) dolomite, (ii) sandy, silty, clayey dolomite, and dolomarl, (iii), dolomitic siltstone and sandstone, (iv) dolomitic limestone, and (v) limestone. In these lithotypes, three types of dolomites are present: non-ferroan replacive, ferroan replacive, and ferroan cement. Fabric retentive and fabric destructive non-ferroan replacive dolomitization are interpreted to have occurred by seepage reflux. Supporting evidence includes the presence gypsum and anhydrite in the Lower Triassic beds. Stable isotope values of the ferroan dolomite (delta O-18 of -10.7 to -4.2 parts per thousand and delta C-13 of 4.8 to 4.7 parts per thousand) suggest dolomitization by fluids of relatively high temperature. The similar stable isotope values (delta O-18 of -9.3 to -5.8 parts per thousand and delta C-13 of -1.9 to 2.5 parts per thousand) of the non-ferroan dolomite phase suggest that the reflux dolomite was overprinted by this second dolomitization event. Traces of exotic minerals, such as barite, chalcopyrite, galena and sulphosalts were found as fillings of vugs and fractures in the dolomite-cemented sandstone. The metals could have been sourced from the underlying Permian red sandstone beds. The heterogeneous sediment composition had profound impact on the diagenesis of these sedimentary successions. LA - English DB - MTMT ER - TY - JOUR AU - Hudáčková, N AU - Holcová, K AU - Halásová, E AU - Kováčová, M AU - Doláková, N AU - Trubač, J AU - Rybár, S AU - Ruman, A AU - Stárek, D AU - Šujan, M AU - Jamrich, M AU - Kováč, M TI - The Pannonian Basin System northern margin paleogeography, climate and depositional environments in the time range during MMCT (Central Paratethys, Novohrad-Nógrád Basin, Slovakia) JF - PALAEONTOLOGIA ELECTRONICA J2 - PALAEONTOL ELECTRON VL - 23 PY - 2020 IS - 3 SN - 1935-3952 DO - 10.26879/1067 UR - https://m2.mtmt.hu/api/publication/31857278 ID - 31857278 N1 - Department of Geology and Paleontology, Faculty of Natural Sciences, Comenius University in Bratislava, Ilkovičova 6, Bratislava, 842 15, Slovakia Institute of Geology and Palaeontology, Charles University, Albertov 6, Prague, 128 43, Czech Republic Masaryk University, Faculty of Science, Department of Geological Sciences, Kotlářská 2, Brno, 611 37, Czech Republic Institute of Geochemistry, Mineralogy and Mineral Resources, Charles University, Albertov 6, Prague, 128 43, Czech Republic Earth Science Institute, Slovak Academy of Sciences, Dúbravská cesta 9, P.O. Box 106, Bratislava, 840 05, Slovakia Cited By :8 Export Date: 30 August 2022 LA - English DB - MTMT ER - TY - JOUR AU - Koroknai, B AU - Wórum, G AU - Tóth, T AU - Koroknai, Zs AU - Fekete-Németh, V AU - Kovács, Gábor TI - Geological deformations in the Pannonian Basin during the neotectonic phase: New insights from the latest regional mapping in Hungary JF - EARTH-SCIENCE REVIEWS J2 - EARTH-SCI REV VL - 211 PY - 2020 PG - 30 SN - 0012-8252 DO - 10.1016/j.earscirev.2020.103411 UR - https://m2.mtmt.hu/api/publication/31640869 ID - 31640869 LA - English DB - MTMT ER - TY - JOUR AU - Kovács, István János AU - Patkó, Levente AU - Liptai, Nóra AU - Lange, Thomas Pieter AU - Taracsák, Z. AU - Cloetingh, S.A.P.L. AU - Török, Kálmán AU - Király, Edit AU - Karátson, Dávid AU - Biró, Tamás AU - Kiss, János AU - Pálos, Zsófia AU - Aradi, László Előd AU - Falus, György AU - Hidas, K. AU - Berkesi, Márta AU - Koptev, A. AU - Novák, Attila AU - Wesztergom, Viktor AU - Fancsik, Tamás AU - Szabó, Csaba TI - The role of water and compression in the genesis of alkaline basalts: Inferences from the Carpathian-Pannonian region JF - LITHOS J2 - LITHOS VL - 354-355 PY - 2020 PG - 16 SN - 0024-4937 DO - 10.1016/j.lithos.2019.105323 UR - https://m2.mtmt.hu/api/publication/31006469 ID - 31006469 N1 - MTA CSFK Lendület Pannon LitH2Oscope Research Group, Sopron, Hungary CSFK Geodetic and Geophysical Institute, Sopron, Hungary Eötvös University, Department of Petrology and Geochemistry, Lithosphere Fluid Research Lab, Budapest, Hungary Institute for Nuclear Research, Isotope Climatology and Environmental Research Centre, Debrecen, Hungary University of Manchester, Department of Earth and Environmental Sciences, Manchester, United Kingdom Utrecht University, Tectonics Research Group, Utrecht, Netherlands Mining and Geological Survey of Hungary, Budapest, Hungary Eötvös University, Department of Physical Geography, Budapest, Hungary Instituto Andaluz de Ciencias de la Tierra, CSIC-UGR, Granada, Spain University of Tübingen, Department of Geosciences, Tübingen, Germany Export Date: 28 May 2021 Correspondence Address: Kovács, I.; MTA CSFK Lendület Pannon LitH2Oscope Research GroupHungary; email: kovacs.istvan.janos@csfk.mta.hu LA - English DB - MTMT ER - TY - JOUR AU - Kovacs, Reka AU - Tamas, Calin Gabriel TI - Cu-3(As,Sb)S-4 minerals from the Baia Mare metallogenic district, Eastern Carpathians, Romania - a case study from the Cisma ore deposit JF - GEOLOGICAL QUARTERLY J2 - GEOL Q VL - 64 PY - 2020 IS - 2 SP - 263 EP - 274 PG - 12 SN - 1641-7291 DO - 10.7306/gq.1529 UR - https://m2.mtmt.hu/api/publication/31415636 ID - 31415636 N1 - Cited By :2 Export Date: 1 July 2022 Correspondence Address: Tãmaş, C.G.; Babeş-Bolyai University, 1 Mihail Kogãlniceanu street, Romania; email: calingtamas@yahoo.fr AB - The occurrence of Cu-3(As,Sb)S-4 minerals, i.e. the enargite and luzonite-famatinite series, is poorly known in the Neogene Baia Mare metallogenic district, NW Romania, with few records and no analytical data. This study provides the first EPMA and XRD data on enargite/luzonite from the Baia Mare metallogenic district, i.e. the Cisma ore deposit from the Mut metallogenic field, and the Herja ore deposit. Vein-type ore bodies bearing Cu-3(As,Sb)S-4 minerals from Cisma are hosted by Paleocene-Eocene flysch successions, while the host rock of the enargite-bearing ore from Herja is unknown. The enargite and luzonite-famatinite series are known as "exotic" in low sulphidation epithermal ore deposits, "typical" in high sulphidation epithermal deposits in association with tennantite, and "sometimes common" in small amounts in intermediate sulphidation epithermal ore deposits. The occurrence of enargite/luzonite in the Baia Mare district suggests the need to update the metal-logenic interpretation for several ore deposits, partly at the district scale in relation to other ore deposit/mineralogy features, e.g. vuggy silica, hypogene argillic alteration. LA - English DB - MTMT ER - TY - JOUR AU - Krstekanić, N AU - Matenco, L AU - Toljić, M AU - Mandić, O AU - Stojadinovic, U AU - Willingshofer, E TI - Understanding partitioning of deformation in highly arcuate orogenic systems: Inferences from the evolution of the Serbian Carpathians JF - GLOBAL AND PLANETARY CHANGE J2 - GLOBAL PLANET CHANGE VL - 195 PY - 2020 SN - 0921-8181 DO - 10.1016/j.gloplacha.2020.103361 UR - https://m2.mtmt.hu/api/publication/31651888 ID - 31651888 N1 - ISSN:0921-8181 LA - English DB - MTMT ER - TY - JOUR AU - Lukoczki, Georgina AU - Haas, János AU - Gregg, JM. AU - Machel, HG. AU - Kele, Sándor AU - John, CM. TI - Early dolomitization and partial burial recrystallization: a case study of Middle Triassic peritidal dolomites in the Villány Hills (SW Hungary) using petrography, carbon, oxygen, strontium and clumped isotope data JF - INTERNATIONAL JOURNAL OF EARTH SCIENCES J2 - INT J EARTH SCI VL - 109 PY - 2020 IS - 3 SP - 1051 EP - 1070 PG - 20 SN - 1437-3254 DO - 10.1007/s00531-020-01851-7 UR - https://m2.mtmt.hu/api/publication/31270514 ID - 31270514 N1 - Funding Agency and Grant Number: American Association of Petroleum Geologists; Geological Society of America Graduate Student Research Grant Program; International Association of Sedimentologists Post-Graduate Grant Scheme; Hungarian Scientific Research FundOrszagos Tudomanyos Kutatasi Alapprogramok (OTKA) [OTKA K124313]; National Research, Development and Innovation Office (NKFIH, Hungary) [KH 125584] Funding text: This work was supported by the American Association of Petroleum Geologists Grants-in-Aid Program, the Geological Society of America Graduate Student Research Grant Program, the International Association of Sedimentologists Post-Graduate Grant Scheme, and the Hungarian Scientific Research Fund (Grant number OTKA K124313). SK was supported by the National Research, Development and Innovation Office (NKFIH, Hungary) (Grant number KH 125584). The authors are indebted to Tamas Budai, Michael Grammer, Gyula Konrad, James Puckette and Pankaj Sarin for their continued help and support. The comments and suggestions of reviewers Arthur Adams and Oliver Weidlich are greatly appreciated. This is an Oklahoma State University Boone Pickens School of Geology contribution #2020-115. AB - Peritidal carbonates of the Csukma Formation (Csukma Dolomite Member) in the Villany Hills, SW Hungary, were investigated to determine the nature of the dolomitization and recrystallization processes that affected these rocks during their complex tectonic evolution, and to evaluate if clumped isotope data preserved signals from the original dolomitization event or are indicative of the later recrystallization processes. Sedimentary and petrographic features, as well as geochemical characteristics integrated with the tectonic evolution of the area indicate that dolomitization likely occurred penecontemporaneously via geothermal convection of normal-to-slightly modified seawater in a near-surface to shallow burial setting. This was followed by partial recrystallization of the dolomites in an intermediate burial setting with low water-to-rock ratios. Results of this study suggest that the clumped isotope temperatures of dolomites, partially recrystallized via dissolution-re-precipitation, may provide a minimum estimate of the temperature of recrystallization. However, caution has to be taken when interpreting the thermal history and fluid evolution of successions that were affected by significant recrystallization, because the clumped isotope temperatures and the calculated fluid compositions might inaccurately represent the diagenetic conditions. LA - English DB - MTMT ER - TY - JOUR AU - Oravecz, Éva AU - Kövér, Szilvia AU - Héja, Gábor AU - Fodor, László TI - Syn-sedimentary and early deformation structures as indications for Jurassic pre-orogenic deformation in the SW Bükk Mts. JF - GEOLOGICA CARPATHICA J2 - GEOL CARPATH VL - 71 PY - 2020 IS - 4 SP - 328 EP - 342 PG - 15 SN - 1335-0552 DO - 10.31577/GeolCarp.71.4.3 UR - https://m2.mtmt.hu/api/publication/31599438 ID - 31599438 N1 - Eötvös Loránd University, Department of Physical and Applied Geology, Pázmány Péter sétány 1/c, Budapest, 1117, Hungary MTA-ELTE Geological, Geophysical and Space Sciences Research Groups, Pázmány Péter sétány 1/c, Budapest, 1117, Hungary Mining and Geological Survey of Hungary, 1145 Budapest, Columbus utca 17, Hungary Export Date: 1 July 2022 Correspondence Address: Oravecz, É.; Eötvös Loránd University, Pázmány Péter sétány 1/c, Hungary; email: orav.eva@gmail.com LA - English DB - MTMT ER - TY - JOUR AU - Patkó, Levente AU - Liptai, Nóra AU - Aradi, László Előd AU - Klébesz, Rita AU - Sendula, Eszter AU - Bodnar, Robert J. AU - Kovács, István János AU - Hidas, Károly AU - Cesare, Bernardo AU - Novák, Attila AU - Trásy, Balázs AU - Szabó, Csaba TI - Metasomatism-induced wehrlite formation in the upper mantle beneath the Nógrád-Gömör Volcanic Field (Northern Pannonian Basin): Evidence from xenoliths JF - GEOSCIENCE FRONTIERS J2 - GEOSCI FRONT VL - 11 PY - 2020 IS - 3 SP - 943 EP - 964 PG - 22 SN - 1674-9871 DO - 10.1016/j.gsf.2019.09.012 UR - https://m2.mtmt.hu/api/publication/31044367 ID - 31044367 N1 - Lithosphere Fluid Research Lab, Institute of Geography and Earth Sciences, Eötvös Loránd University, Budapest, Hungary Isotope Climatology and Environmental Research Centre, Institute for Nuclear Research, Hungarian Academy of Sciences, Debrecen, Hungary CCFS-GEMOC, Department of Earth and Planetary Sciences, Macquarie University, Sydney, Australia Geodetic and Geophysical Institute, Research Centre for Astronomy and Earth Sciences, Hungarian Academy of Sciences, Sopron, Hungary Fluids Research Laboratory, Department of Geosciences, Virginia Tech, Blacksburg, VA, United States MTA CSFK Lendület Pannon LitH2Oscope Research Group, Geodetic and Geophysical Institute, Research Centre for Astronomy and Earth Sciences, Hungarian Academy of Sciences, Sopron, Hungary Instituto Andaluz de Ciencias de La Tierra, CSIC & UGR, Armilla, Granada, Spain Department of Geosciences, University of Padua, Padua, Italy Department of Geology, Eötvös Loránd University, Budapest, Hungary Export Date: 28 May 2021 Correspondence Address: Szabó, C.; Lithosphere Fluid Research Lab, Hungary; email: cszabo@elte.hu LA - English DB - MTMT ER - TY - JOUR AU - Plasienka, Dusan AU - Bucova, Jana AU - Simonova, Viera TI - Variable structural styles and tectonic evolution of an ancient backstop boundary: the Pieniny Klippen Belt of the Western Carpathians JF - INTERNATIONAL JOURNAL OF EARTH SCIENCES J2 - INT J EARTH SCI VL - 109 PY - 2020 IS - 4 SP - 1355 EP - 1376 PG - 22 SN - 1437-3254 DO - 10.1007/s00531-019-01789-5 UR - https://m2.mtmt.hu/api/publication/31422844 ID - 31422844 N1 - Department of Geology and Palaeontology, Faculty of Natural Sciences, Comenius University, Mlynská dolina, Ilkovičova 6, Bratislava, 842 15, Slovakia Earth Science Institute, Slovak Academy of Sciences, Dúbravská cesta 9, P.O. Box 106, Bratislava, 840 05, Slovakia DPP Žilina Ltd, Legionárska 8203, Žilina, 010 01, Slovakia Department of Geography and Geology, Faculty of Natural Sciences, Matej Bel University, Tajovského 40, Banská Bystrica, 974 01, Slovakia Cited By :13 Export Date: 1 July 2022 CODEN: IJESF Correspondence Address: Plašienka, D.; Department of Geology and Palaeontology, Mlynská dolina, Ilkovičova 6, Slovakia; email: dusan.plasienka@uniba.sk AB - The Pieniny Klippen Belt (PKB) and adjoining zones form a narrow, but lengthy belt that separates the Cretaceous nappe stack of the Central (Austroalpine) and the Cenozoic accretionary wedge of the External Western Carpathians (Flysch Belt). The PKB shares units and structures of both, in addition to the distinctive Oravic units, derived from a continental fragment in the Middle Penninic position. In map view, the northward-convex PKB consists of two branches-the western one striking roughly SW-NE and the eastern one oriented in the NW-SE direction. The western branch experienced a continuous NW-SE convergence and forward accretion of units derived from the foreland plate during the Late Cretaceous up to Oligocene. The developing accretionary wedge was supported by the backstop of the Central Carpathians. In contrast, the eastern branch originated by separation of PKB units and their dextral translation along the NE margin of the Central Carpathian block in the Late Eocene. During the Miocene reorganization of plate movements in the Carpathian area, the situation reversed. The eastern, formerly dextral transform margin was converted to the frontal backstop of the eastern part of the accretionary wedge. In contrast, the western, previously orthogonally convergent branch was affected by along-strike sinistral movements. Despite these considerable kinematic changes, the PKB remained fixed to both backstop edges and records deformation structures and associated sediments differentiated into several evolutionary stages. LA - English DB - MTMT ER - TY - JOUR AU - Rybak-Ostrowska, Barbara AU - Gasinski, Arkadiusz AU - Kapron, Grzegorz TI - Dawsonite as an indicator of multistage deformation and fluid pathways within fault zones: Insights from the Fore-Dukla Thrust Sheet, Outer Carpathians, Poland JF - ACTA GEOLOGICA POLONICA J2 - ACTA GEOL POL VL - 70 PY - 2020 IS - 1 SP - 51 EP - 78 PG - 28 SN - 0001-5709 DO - 10.24425/agp.2019.126453 UR - https://m2.mtmt.hu/api/publication/31437030 ID - 31437030 N1 - Faculty of Geology, University of Warsaw, Żwirki i Wigury 93, Warsaw, 02-089, Poland Institute of Ceramics and Building Materials, Postępu 9, Warsaw, 02-676, Poland Export Date: 1 July 2022 Correspondence Address: Rybak-Ostrowska, B.; Faculty of Geology, Żwirki i Wigury 93, Poland; email: barbara.rybak@uw.edu.pl AB - The structural pattern developed within metre to microscopic scale thrust and strike-slip fault zones exposed in the Palaeogene flysch rocks of the Fore-Dukla Thrust Sheet in the south-eastern part of the Silesian Nappe, Outer Carpathians, Poland, reveals evidence for upper crustal deformation and fluid flow. Syntectonic dawsonite [NaAlCO3(OH)(2)] indicates the following series of deformational events within the fault zones: i) detachment and buckle folding resulting from movement along thrust faults; ii) faulting as a compensation of the shortening, resulting in the fault propagation folding, breakthrough thrust faulting and imbrications; and iii) strike-slip faulting. The microstructural pattern coupled with the growth of a related sequence of carbonate minerals within the fault zones, followed by present-day dawsonite precipitation and tufa formation, indicate a continuing influence of fluids within the Silesian Nappe up to and including modem time. Structural observations at metre to microscopic scales coupled with EDS mapping of rocks indicate that dawsonite is a unique tool for the reconstruction of subsequent deformation in the Fore-Dukla Thrust Sheet. LA - English DB - MTMT ER - TY - JOUR AU - Starostenko, Vitaly AU - Janik, Tomasz AU - Mocanu, Victor AU - Stephenson, Randell AU - Yegorova, Tamara AU - Amashukeli, Tatiana AU - Czuba, Wojciech AU - Środa, Piotr AU - Murovskaya, Anna AU - Kolomiyets, Katerina AU - Lysynchuk, Dmytro AU - Okoń, Jan AU - Dragut, Alina AU - Omelchenko, Victor AU - Legostaieva, Olga AU - Gryn, Dmytro AU - Mechie, James AU - Tolkunov, Anatoly TI - RomUkrSeis: Seismic model of the crust and upper mantle across the Eastern Carpathians – From the Apuseni Mountains to the Ukrainian Shield JF - TECTONOPHYSICS J2 - TECTONOPHYSICS VL - 794 PY - 2020 SP - 1 EP - 28 PG - 28 SN - 0040-1951 DO - 10.1016/j.tecto.2020.228620 UR - https://m2.mtmt.hu/api/publication/31646899 ID - 31646899 N1 - Institute of Geophysics, National Academy of Sciences of Ukraine, Kiev, Ukraine Institute of Geophysics, Polish Academy of Sciences, Warsaw, Poland University of Bucharest, Romania School of Geosciences, University of Aberdeen Deutsches GeoForschungsZentrum – GFZ, Section “Geophysical Deep Sounding”, Telegrafenberg, Potsdam, 14473, Germany Ukrgeofizika, Kiev, Ukraine Cited By :4 Export Date: 30 June 2022 Correspondence Address: Stephenson, R.; School of Geosciences, email: r.stephenson@abdn.ac.uk LA - English DB - MTMT ER - TY - JOUR AU - Baranyi, Viktória AU - Rostási, Ágnes AU - Raucsik, Béla AU - Kürschner, WM TI - Palynology and weathering proxies reveal climatic fluctuations during the Carnian Pluvial Episode (CPE) (late Triassic) from marine successions in the Transdanubian Range (western Hungary) JF - GLOBAL AND PLANETARY CHANGE J2 - GLOBAL PLANET CHANGE VL - 177 PY - 2019 SP - 157 EP - 172 PG - 16 SN - 0921-8181 DO - 10.1016/j.gloplacha.2019.01.018 UR - https://m2.mtmt.hu/api/publication/30626415 ID - 30626415 N1 - Department of Geosciences, University of Oslo, P.O. Box 1047, Blindern, Oslo, 0316, Norway Department of Earth and Environmental Sciences, University of Pannonia, P.O.Box 158, Veszprém, H-8201, Hungary Department of Mineralogy, Geochmistry, and Geochemistry, University of Szeged, Egyetem utca 2–6, Szeged, H-6722, Hungary Cited By :9 Export Date: 1 July 2022 CODEN: GPCHE Correspondence Address: Baranyi, V.; Department of Geosciences, P.O. Box 1047, Blindern, Norway; email: viktoria.baranyi@geo.uio.no LA - English DB - MTMT ER - TY - JOUR AU - Bónová, Katarína AU - Bóna, Ján AU - Pańczyk, Magdalena AU - Kováčik, Martin AU - Mikuš, Tomáš AU - Laurinc, Dušan TI - Origin of deep-sea clastics of the Magura Basin (Eocene Makovica sandstones in the Outer Western Carpathians) with constraints of framework petrography, heavy mineral analysis and zircon geochronology JF - PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY J2 - PALAEOGEOGR PALAEOCL VL - 514 PY - 2019 SP - 768 EP - 784 PG - 17 SN - 0031-0182 DO - 10.1016/j.palaeo.2018.09.025 UR - https://m2.mtmt.hu/api/publication/30371245 ID - 30371245 N1 - Institute of Geography, Faculty of Science, Pavol Jozef Šafárik University in Košice, Jesenná 5, Košice, 040 01, Slovakia Polish Geological Institute – National Research Institute, 4 Rakowiecka St., Warszawa, 00-975, Poland Earth Science Institute, Slovak Academy of Sciences, Geological Division, Ďumbierska 1, Banská Bystrica, 974 01, Slovakia State Geological Institute of Dionýz Štúr, Mlynská dolina 1, Bratislava, 817 04, Slovakia Export Date: 10 January 2019 CODEN: PPPYA Correspondence Address: Bónová, K.; Institute of Geography, Faculty of Science, Pavol Jozef Šafárik University in Košice, Jesenná 5, Slovakia; email: katarina.bonova@upjs.sk LA - English DB - MTMT ER - TY - JOUR AU - Caporali, A. AU - Zurutuza, J. AU - Bertocco, M. AU - Ishchenko, M. AU - Khoda, O. TI - Present day geokinematics of Central Europe JF - JOURNAL OF GEODYNAMICS J2 - J GEODYN VL - 132 PY - 2019 SN - 0264-3707 DO - 10.1016/j.jog.2019.101652 UR - https://m2.mtmt.hu/api/publication/30916695 ID - 30916695 N1 - Università di Padova, Dipartimento di Geoscienze, Padova, Italy Main Astronomical Observatory, National Academy of Sciences, Kiev, Ukraine Cited By :4 Export Date: 14 February 2022 Correspondence Address: Caporali, A.; Università di Padova, Italy; email: alessandro.caporali@unipd.it LA - English DB - MTMT ER - TY - JOUR AU - Dererova, Jana AU - Bielik, Miroslav AU - Kohut, Igor AU - Godova, Dominika TI - Calculation of temperature distribution and rheological properties of the lithosphere along transect IV in the Western Carpathian-Pannonian Basin region JF - CONTRIBUTIONS TO GEOPHYSICS AND GEODESY J2 - CONTRIB GEOPHYS GEODES VL - 49 PY - 2019 IS - 4 SP - 497 EP - 510 PG - 14 SN - 1335-2806 DO - 10.2478/congeo-2019-0026 UR - https://m2.mtmt.hu/api/publication/31046757 ID - 31046757 N1 - Division of Geophysics, Earth Science Institute, Slovak Academy of Sciences, Dúbravská cesta 9, Bratislava, 840 05, Slovakia Department of Applied and Environmental Geophysics, Faculty of Natural Sciences, Comenius University, Mlynská Dolina, Ilkovičova 6, Bratislava, 842 48, Slovakia Cited By :1 Export Date: 1 July 2022 Correspondence Address: Dérerová, J.; Division of Geophysics, Dúbravská cesta 9, Slovakia; email: geofjade@savba.sk AB - 2D integrated modelling algorithm was used to calculate the temperature distribution in the lithosphere along the transect IV located in the Western Carpathian-Pannonian Basin area. Based on the determined temperature field and given rheological parameters of the rocks, it was possible to calculate the strength distribution for both compressional and extensional regimes, construct the strength envelopes for chosen columns of the main tectonic units of the model, and thus construct a simple rheological model of the lithosphere along transect IV. The obtained results indicate decrease of the lithospheric strength from the European platform and the Western Carpathians towards the Pannonian Basin. The largest strength (valid for all tectonic units) can be observed within the upper crust with its maxima on the boundary between upper and lower crust, decreasing towards lower crust and disappearing in the lithospheric mantle, suggesting mostly rigid deformation occurring in the upper crust. A local increase in the values of strength can be observed in the eastern segment of the Western Carpathians where crustal thickening accompanies the lithospheric thickening (formation of the lithospheric root), unlike the previous models along transects I and II, that pass through the western segment of the Western Carpathians and their lithosphere-asthenosphere boundary is almost flat and therefore no accompanying crustal thickening is observed and the decrease in strength is slow and steady. LA - English DB - MTMT ER - TY - JOUR AU - Fodor, László TI - Results, problems and future tasks of palaeostress and fault-slip analyses in the Pannonian Basin: the Hungarian contribution JF - FÖLDTANI KÖZLÖNY J2 - FÖLDTANI KÖZLÖNY VL - 149 PY - 2019 IS - 4 SP - 297 EP - 326 PG - 30 SN - 0015-542X DO - 10.23928/foldt.kozl.2019.149.4.297 UR - https://m2.mtmt.hu/api/publication/30852034 ID - 30852034 N1 - Export Date: 27 November 2019 Correspondence Address: Fodor, L.; MTA-ELTE Geological, Geophysical and Space Science Research Group, Pázmány P. sétány 1/C, Hungary; email: lasz.Fodor@yahoo.com LA - English DB - MTMT ER - TY - JOUR AU - Golonka, Jan AU - Pietsch, Kaja AU - Marzec, Paweł AU - Kasperska, Monika AU - Dec, Jerzy AU - Cichostępski, Kamil AU - Lasocki, Stanisław TI - Deep structure of the Pieniny Klippen Belt in Poland JF - SWISS JOURNAL OF GEOSCIENCES J2 - SWISS J GEOSCI VL - 112 PY - 2019 IS - 2-3 SP - 475 EP - 506 PG - 32 SN - 1661-8726 DO - 10.1007/s00015-019-00345-2 UR - https://m2.mtmt.hu/api/publication/31029211 ID - 31029211 N1 - AGH University of Science and Technology, Faculty of Geology, Geophysics and Environmental Protection, ul. Mickiewicza 30, Kraków, 30-059, Poland Institute of Geophysics, Polish Academy of Sciences, ul. Księcia Janusza 64, Warsaw, 01-452, Poland Cited By :14 Export Date: 30 June 2022 Correspondence Address: Golonka, J.; AGH University of Science and Technology, ul. Mickiewicza 30, Poland; email: jgolonka@agh.edu.pl LA - English DB - MTMT ER - TY - JOUR AU - Harangi, Szabolcs AU - Haranginé Lukács, Réka TI - A Kárpát-Pannon térség neogén-kvarter vulkanizmusa és geodinamikai kapcsolata JF - FÖLDTANI KÖZLÖNY J2 - FÖLDTANI KÖZLÖNY VL - 149 PY - 2019 IS - 3 SP - 197 EP - 232 PG - 36 SN - 0015-542X DO - 10.23928/foldt.kozl.2019.149.3.197 UR - https://m2.mtmt.hu/api/publication/30855045 ID - 30855045 N1 - A szerzők egyenlő mértékben járultak hozzá az összefoglaló kézirat elkészítéséhez. LA - Hungarian DB - MTMT ER - TY - JOUR AU - Jankovics, M. Éva AU - Sági, Tamás AU - Astbury, R.L. AU - Petrelli, M. AU - Kiss, Balázs AU - Ubide, T. AU - Németh, Károly AU - Ntaflos, T. AU - Harangi, Szabolcs TI - Olivine major and trace element compositions coupled with spinel chemistry to unravel the magmatic systems feeding monogenetic basaltic volcanoes JF - JOURNAL OF VOLCANOLOGY AND GEOTHERMAL RESEARCH J2 - J VOLCANOL GEOTH RES VL - 369 PY - 2019 SP - 203 EP - 223 PG - 21 SN - 0377-0273 DO - 10.1016/j.jvolgeores.2018.11.027 UR - https://m2.mtmt.hu/api/publication/30350207 ID - 30350207 N1 - MTA-ELTE Volcanology Research Group, Pázmány Péter sétány 1/C, Budapest, 1117, Hungary Department of Petrology and Geochemistry, Eötvös Loránd University, Pázmány Péter sétány 1/C, Budapest, 1117, Hungary Petro-Volcanology Research Group, Department of Physics and Geology, Università degli Studi di Perugia, Piazza dell'Università 1, Perugia, 06123, Italy Institute of Geography and Earth Sciences, Eötvös Loránd University, Pázmány Péter sétány 1/C, Budapest, 1117, Hungary School of Earth and Environmental Sciences, The University of Queensland, Brisbane, QLD 4072, Australia Institute of Agriculture and Environment, Massey University, Private Bag 11222, Palmerston North, New Zealand Department of Lithospheric Research, University of Vienna, Althanstrasse 14, Vienna, 1090, Austria Export Date: 17 December 2018 Funding Agency and Grant Number: European Union; State of Hungary; European Social Fund [TAMOP 4.2.4. A/2-11-1-2012-0001]; Hungarian-Austrian Cooperation [TET_10-1-2011-0694]; Collegium Hungaricum scholarship of the Balassi Institute; Erasmus + programme (2017-2019 Erasmus+ ICM, ELTE-Massey University) of the European Union Funding text: We are grateful to Lucy E. McGee and Marco Brenna for their constructive reviews, valuable suggestions and comments which helped to improve the first version of the manuscript. In this research, M. Eva Jankovics was partly supported by the European Union and the State of Hungary, co-financed by the European Social Fund in the framework of TAMOP 4.2.4. A/2-11-1-2012-0001 'National Excellence Program'. The TET_10-1-2011-0694 project (Hungarian-Austrian Cooperation) as well as the Collegium Hungaricum scholarship of the Balassi Institute provided partial financial support. Zsolt Bendo and Franz Kiraly are acknowledged for their help during the SEM and EMPA analyses. Cooperation of Karoly Nemeth and Tams Sagi was supported by the Erasmus + programme (2017-2019 Erasmus+ ICM, ELTE-Massey University) of the European Union. LA - English DB - MTMT ER - TY - JOUR AU - Kalmár, Dániel AU - Hetényi, György AU - Bondár, István TI - Moho depth analysis of the eastern Pannonian Basin and the Southern Carpathians from receiver functions JF - JOURNAL OF SEISMOLOGY J2 - J SEISMOL VL - 23 PY - 2019 IS - 5 SP - 967 EP - 982 PG - 16 SN - 1383-4649 DO - 10.1007/s10950-019-09847-w UR - https://m2.mtmt.hu/api/publication/30738360 ID - 30738360 N1 - Export Date: 15 July 2019 CODEN: DXUEF Correspondence Address: Kalmár, D.; Department of Geophysics and Space Science, Eötvös Loránd UniversityHungary; email: kaduaat@caesar.elte.hu Funding Agency and Grant Number: Eotvos Lorand University (ELTE); National Research, Development and Innovation Fund [K124241, 2018-1.2.1-NKP-201800007, K128152] Funding text: Open access funding provided by Eotvos Lorand University (ELTE). The reported investigation was financially supported by the National Research, Development and Innovation Fund (Grant Nos. K124241; 2018-1.2.1-NKP-201800007 and K128152). Export Date: 8 January 2021 CODEN: DXUEF Correspondence Address: Kalmár, D.; Department of Geophysics and Space Science, Eötvös Loránd UniversityHungary; email: kaduaat@caesar.elte.hu Funding details: National Eye Research Centre, NERC Funding details: University of Leeds Funding text 1: We greatly acknowledge the scientific and field teams of the South Carpathian Project, which was founded by NERC (UK) and lead by the University of Leeds. We acknowledge the authors of Generic Mapping Tools (GMT) software (Wessel and Smith 1998). The authors are grateful to Marek Grad for his constructive review and for sharing data for Fig. 9b and to an anonymous reviewer whose comments helped to improve the paper. Export Date: 16 February 2021 CODEN: DXUEF Correspondence Address: Kalmár, D.; Department of Geophysics and Space Science, Hungary; email: kaduaat@caesar.elte.hu Funding details: National Eye Research Centre, NERC Funding details: University of Leeds Funding text 1: We greatly acknowledge the scientific and field teams of the South Carpathian Project, which was founded by NERC (UK) and lead by the University of Leeds. We acknowledge the authors of Generic Mapping Tools (GMT) software (Wessel and Smith 1998). The authors are grateful to Marek Grad for his constructive review and for sharing data for Fig. 9b and to an anonymous reviewer whose comments helped to improve the paper. LA - English DB - MTMT ER - TY - JOUR AU - Kis, Boglárka Mercédesz AU - Caracausi, A. AU - Palcsu, László AU - Baciu, C. AU - Ionescu, Artur AU - Futó, István AU - Sciarra, A. AU - Harangi, Szabolcs TI - Noble gas and carbon isotope systematics at the seemingly inactive Ciomadul volcano (Eastern‐Central Europe, Romania): evidence for volcanic degassing JF - GEOCHEMISTRY GEOPHYSICS GEOSYSTEMS J2 - GEOCHEM GEOPHY GEOSY VL - 20 PY - 2019 IS - 6 SP - 3019 EP - 3043 PG - 25 SN - 1525-2027 DO - 10.1029/2018GC008153 UR - https://m2.mtmt.hu/api/publication/30727878 ID - 30727878 N1 - Funding Agency and Grant Number: OTKA (Hungarian National Research Fund) [K116528]; European Union; State of Hungary; European Regional Development Fund [GINOP-2.3.2-15-2016-00009]; Deep Energy Community and Reservoirs and Fluxes Community of the Deep Carbon Observatory Funding text: Information regarding the support of the conclusions of this work can be found in the tables and within the text. This research on the Ciomadul volcano was initiated during the MTA Postdoctoral Fellowship of Boglarka-Mercedesz Kis and belongs to the scientific project supported by the OTKA (Hungarian National Research Fund) K116528. The research was also supported by the European Union and the State of Hungary, cofinanced by the European Regional Development Fund in the project of GINOP-2.3.2-15-2016-00009 "ICER," and we acknowledge the support of the Deep Energy Community and Reservoirs and Fluxes Community of the Deep Carbon Observatory. Thorough reviews and constructive comments provided by Emilie Roulleau and Daniele Pinti helped considerably to clarify the ideas described in the paper. We thank Timothy Jull who provided a final polishing of the English of the manuscript. LA - English DB - MTMT ER - TY - JOUR AU - Lange, Thomas Pieter AU - Szabó, Csaba AU - Liptai, Nóra AU - Patkó, Levente AU - Gelencsér, Orsolya AU - Aradi, László Előd AU - Kovács, István János TI - A földköpeny reológiai kutatása: mennyiségi Fourier transzformációs infravörös spektrometria alkalmazása egy Persány hegységi xenolit példáján JF - FÖLDTANI KÖZLÖNY J2 - FÖLDTANI KÖZLÖNY VL - 149 PY - 2019 IS - 3 SP - 233 EP - 254 PG - 22 SN - 0015-542X DO - 10.23928/foldt.kozl.2019.149.3.233 UR - https://m2.mtmt.hu/api/publication/30850025 ID - 30850025 N1 - Eötvös Loránd Tudományegyetem, Földrajz-és Földtudományi Intézet, Litoszféra Fluidum Kutató Laboratórium (LRG), Pázmány Péter sétány 1/c, Budapest, H-1117, Hungary MTA CSFK Lendület Pannon LitH2 Oscope Lendület Kutatócsoport, Hungary MTA CSFK Geofizika és Geodéziai Intézet, Csatkai Endre u. 6–8, Sopron, H–9400, Hungary MTA Atommagkutató Intézet, Izotóp Klimatológiai és Környezetkutató Központ (IKER), Bem tér 18/c, Debrecen, H–4026, Hungary Cited By :3 Export Date: 16 February 2021 Correspondence Address: Lange, T.P.; Eötvös Loránd Tudományegyetem, Pázmány Péter sétány 1/c, Hungary; email: lange.thomas@hotmail.com Funding details: Magyar Tudományos Akadémia, MTA Funding text 1: A szerz?k k?sz?nik az LRG tagok k?zrem?k?d?s?t, k?-l?n?sen P?LOS Zs?fia ?nzetlen seg?ts?g?t. Az FT?IR m?r?-sek kivitelez?s?ben ny?jtott seg?ts?g?rt k?sz?net illeti KESJ?R D?r?t (MTA CSFK FGI). LANGE Thomas Pieter k?sz?ni az Emberi Er?forr?sok Miniszt?riuma ?NKP-18-3 k?dsz?m? ?j Nemzeti Kiv?l?-s?g Programj?nak t?mogat?s?t, amely hozz?j?rult a dol-gozat elk?sz?t?s?hez. ARADI L?szl? k?sz?ni az ELTE Fels?oktat?si Int?zm?-nyi Kiv?l?s?gi Program (1783-3/2018/FEKUTSRAT) nev? p?ly?zat t?mogat?s?t, amely az Emberi Er?forr?sok Miniszt?riuma t?mogat?s?val val?sult meg. A k?zirat elk?-sz?lt?t t?mogatta az MTA CSFK Lend?let Pannon LitH2 Oscope Kutat?csoport. A cikk az LRG 97. publik?ci?ja, amely a MTA CSFK GGI ?s a Lend?let Pannon LitH2 Oscope Kutat?csoportj?val egy?ttm?k?d?sben k?sz?lt. A szerz?k k?sz?nik BAL?ZS Attil?nak ?s az Anonim b?r?l?knak a k?zirat olvas?sa sor?n tett jav?t?saikat ?s hasz-nos javaslataikat/tan?csaikat. LA - Hungarian DB - MTMT ER - TY - JOUR AU - Leskó, Máté Zsigmond AU - Papp, Richárd Zoltán AU - Topa, Boglárka Anna AU - Kristály, Ferenc AU - Vigh, Tamás AU - Zajzon, Norbert TI - Smectite appearance in the footwall of the Úrkút manganese ore deposit, Bakony Mts., Hungary JF - CENTRAL EUROPEAN GEOLOGY J2 - CENT EUR GEOL VL - 62 ET - 0 PY - 2019 IS - 1 SP - 100 EP - 118 PG - 19 SN - 1788-2281 DO - 10.1556/24.62.2019.02 UR - https://m2.mtmt.hu/api/publication/30415355 ID - 30415355 N1 - "A cikkben/előadásban/tanulmányban ismertetett kutató munka az EFOP-3.6.1-16-2016-00011 jelű „Fiatalodó és Megújuló Egyetem – Innovatív Tudásváros – a Miskolci Egyetem intelligens szakosodást szolgáló intézményi fejlesztése” projekt részeként – a Széchenyi 2020 keretében – az Európai Unió támogatásával, az Európai Szociális Alap társfinanszírozásával valósul meg" = “The described article/presentation/study was carried out as part of the EFOP-3.6.1-16-2016-00011 “Younger and Renewing University – Innovative Knowledge City – institutional development of the University of Miskolc aiming at intelligent specialisation” project implemented in the framework of the Szechenyi 2020 program. The realization of this project is supported by the European Union, co-financed by the European Social Fund.” LA - English DB - MTMT ER - TY - JOUR AU - Liptai, Nóra AU - Hidas, K. AU - Tommasi, A. AU - Patkó, Levente AU - Kovács, István János AU - Griffin, W.L. AU - O'Reilly, S.Y. AU - Pearson, N.J. AU - Szabó, Csaba TI - Lateral and vertical heterogeneity in the lithospheric mantle at the northern margin of the Pannonian Basin reconstructed from peridotite xenolith microstructures JF - JOURNAL OF GEOPHYSICAL RESEARCH: SOLID EARTH J2 - J GEOPHYS RES SOLID EARTH VL - 124 PY - 2019 IS - 7 SP - 6315 EP - 6336 PG - 22 SN - 2169-9313 DO - 10.1029/2018JB016582 UR - https://m2.mtmt.hu/api/publication/30706849 ID - 30706849 N1 - Funding Agency and Grant Number: Marie Curie International Reintegration Grant [NAMS-230937]; Bolyai Janos Postdoctoral Research Fellowship of the Hungarian Academy of Sciences; Lendulet Pannon LitH2Oscope Research Group (Research Centre for Astronomy and Earth Sciences, Hungarian Academy of Sciences); Macquarie University international PhD scholarship; ARC Centre of Excellence for Core to Crust Fluid Systems (CCFS); Ministry of Economy, Industry and Competitiveness (MINECO, Spain); State Research Agency (AEI, Spain) [FPDI-2013-16253, CGL2016-81085-R]; DEST Systemic Infrastructure Grants; ARC LIEF; NCRIS/AuScope; Macquarie University; Hungarian Scientific Research Fund (OTKA) [PD101683] Funding text: The authors would like to thank the people who contributed to this work. We owe thanks to Fabrice Barou and David Adams for their help with EBSDSEM analyses at Geosciences Montpellier and at CCFS Macquarie University, respectively. Laszlo Aradi is acknowledged for his help with field work, petrography and MTEX application. We are grateful for the constructive criticism of Sandra Piazolo and Jacques Precigout and two anonymous reviewers, as well as for the editorial handling of Stephen Parman. Our research received financial support from a Marie Curie International Reintegration Grant (grant NAMS-230937), a postdoctoral grant (grant PD101683) of the Hungarian Scientific Research Fund (OTKA), and a Bolyai Janos Postdoctoral Research Fellowship of the Hungarian Academy of Sciences to I. J. K., as well as from the Lendulet Pannon LitH2Oscope Research Group (Research Centre for Astronomy and Earth Sciences, Hungarian Academy of Sciences). N. L. received support from Macquarie University international PhD scholarship and project and travel funding from ARC Centre of Excellence for Core to Crust Fluid Systems (CCFS). K. H. acknowledges funding from Ministry of Economy, Industry and Competitiveness (MINECO, Spain) and the State Research Agency (AEI, Spain; grants FPDI-2013-16253 and CGL2016-81085-R). Instruments used at Macquarie University are funded by DEST Systemic Infrastructure Grants, ARC LIEF, NCRIS/AuScope, industry partners, and Macquarie University. The data used in this paper are listed in the references, tables, and supporting information. The raw EBSD data are available from the corresponding author upon request. This is the 92nd publication of the Lithosphere Fluid Research Lab (LRG), contribution 1361 from the ARC Centre of Excellence for Core to Crust Fluid Systems (www.ccfs.mq.edu.au) and 1320 from the GEMOC Key Centre (www.gemoc.mq.edu.au). Funding Agency and Grant Number: Marie Curie International Reintegration GrantEuropean Union (EU) [NAMS-230937]; Bolyai Janos Postdoctoral Research Fellowship of the Hungarian Academy of Sciences; Lendulet Pannon LitH2Oscope Research Group (Research Centre for Astronomy and Earth Sciences, Hungarian Academy of Sciences); Macquarie University international PhD scholarship; ARC Centre of Excellence for Core to Crust Fluid Systems (CCFS)Australian Research Council; Ministry of Economy, Industry and Competitiveness (MINECO, Spain); State Research Agency (AEI, Spain) [FPDI-2013-16253, CGL2016-81085-R]; DEST Systemic Infrastructure GrantsAustralian GovernmentDepartment of Industry, Innovation and Science; ARC LIEFAustralian Research Council; NCRIS/AuScopeAustralian GovernmentDepartment of Industry, Innovation and Science; Macquarie University; Hungarian Scientific Research Fund (OTKA)Orszagos Tudomanyos Kutatasi Alapprogramok (OTKA) [PD101683] Funding text: The authors would like to thank the people who contributed to this work. We owe thanks to Fabrice Barou and David Adams for their help with EBSDSEM analyses at Geosciences Montpellier and at CCFS Macquarie University, respectively. Laszlo Aradi is acknowledged for his help with field work, petrography and MTEX application. We are grateful for the constructive criticism of Sandra Piazolo and Jacques Precigout and two anonymous reviewers, as well as for the editorial handling of Stephen Parman. Our research received financial support from a Marie Curie International Reintegration Grant (grant NAMS-230937), a postdoctoral grant (grant PD101683) of the Hungarian Scientific Research Fund (OTKA), and a Bolyai Janos Postdoctoral Research Fellowship of the Hungarian Academy of Sciences to I. J. K., as well as from the Lendulet Pannon LitH2Oscope Research Group (Research Centre for Astronomy and Earth Sciences, Hungarian Academy of Sciences). N. L. received support from Macquarie University international PhD scholarship and project and travel funding from ARC Centre of Excellence for Core to Crust Fluid Systems (CCFS). K. H. acknowledges funding from Ministry of Economy, Industry and Competitiveness (MINECO, Spain) and the State Research Agency (AEI, Spain; grants FPDI-2013-16253 and CGL2016-81085-R). Instruments used at Macquarie University are funded by DEST Systemic Infrastructure Grants, ARC LIEF, NCRIS/AuScope, industry partners, and Macquarie University. The data used in this paper are listed in the references, tables, and supporting information. The raw EBSD data are available from the corresponding author upon request. This is the 92nd publication of the Lithosphere Fluid Research Lab (LRG), contribution 1361 from the ARC Centre of Excellence for Core to Crust Fluid Systems (www.ccfs.mq.edu.au) and 1320 from the GEMOC Key Centre (www.gemoc.mq.edu.au). Lithosphere Fluid Research Lab, Institute of Geography and Earth Sciences, Eötvös University, Budapest, Hungary Australian Research Council Centre of Excellence for Core to Crust Fluid Systems and GEMOC, Department of Earth and Planetary Sciences, Macquarie University, North Ryde, NSW, Australia Now at MTA CSFK Lendület Pannon LitH2Oscope Research Group, MTA Research Centre for Astronomy and Earth Sciences, Sopron, Hungary Instituto Andaluz de Ciencias de la Tierra, CSIC and UGR, Armilla, Spain Departamento de Geodinámica, Universidad de Granada, Granada, Spain Géosciences Montpellier, Université de Montpellier and CNRS, CC 60, Montpellier, cedex 5, France Geodetic and Geophysical Institute, MTA Research Centre for Astronomy and Earth Sciences, Sopron, Hungary MTA CSFK Lendület Pannon LitH2Oscope Research Group, MTA Research Centre for Astronomy and Earth Sciences, Sopron, Hungary Cited By :7 Export Date: 16 February 2021 Correspondence Address: Szabó, C.; Lithosphere Fluid Research Lab, Hungary; email: cszabo@elte.hu Funding details: 1320 Funding details: Australian Education International, Australian Government, AEI, CGL2016-81085-R, FPDI-2013-16253 Funding details: Centre of Excellence for Core to Crust Fluid Systems, Australian Research Council, CCFS, ARC Funding details: Macquarie University Funding details: Ministerio de Economía y Competitividad, MINECO Funding details: Hungarian Scientific Research Fund, OTKA Funding details: Magyar Tudományos Akadémia, MTA Funding details: Ministerio de Economía, Industria y Competitividad, Gobierno de España, MINECO Funding details: Geochemical Evolution and Metallogeny of Continents, GEMOC Funding text 1: The authors would like to thank the people who contributed to this work. We owe thanks to Fabrice Barou and David Adams for their help with EBSD-SEM analyses at Geosciences Montpellier and at CCFS Macquarie University, respectively. L?szl? Aradi is acknowledged for his help with field work, petrography and MTEX application. We are grateful for the constructive criticism of Sandra Piazolo and Jacques Pr?cigout and two anonymous reviewers, as well as for the editorial handling of Stephen Parman. Our research received financial support from a Marie Curie International Reintegration Grant (grant NAMS-230937), a postdoctoral grant (grant PD101683) of the Hungarian Scientific Research Fund (OTKA), and a Bolyai J?nos Postdoctoral Research Fellowship of the Hungarian Academy of Sciences to I. J. K., as well as from the Lend?let Pannon LitH2Oscope Research Group (Research Centre for Astronomy and Earth Sciences, Hungarian Academy of Sciences). N. L. received support from Macquarie University international PhD scholarship and project and travel funding from ARC Centre of Excellence for Core to Crust Fluid Systems (CCFS). K. H. acknowledges funding from Ministry of Economy, Industry and Competitiveness (MINECO, Spain) and the State Research Agency (AEI, Spain; grants FPDI-2013-16253 and CGL2016-81085-R). Instruments used at Macquarie University are funded by DEST Systemic Infrastructure Grants, ARC LIEF, NCRIS/AuScope, industry partners, and Macquarie University. The data used in this paper are listed in the references, tables, and supporting information. The raw EBSD data are available from the corresponding author upon request. This is the 92nd publication of the Lithosphere Fluid Research Lab (LRG), contribution 1361 from the ARC Centre of Excellence for Core to Crust Fluid Systems (www.ccfs.mq.edu.au) and 1320 from the GEMOC Key Centre (www.gemoc.mq.edu.au). LA - English DB - MTMT ER - TY - JOUR AU - Ludwiniak, Miroslaw AU - Smigielski, Michal AU - Kowalczyk, Sebastian AU - Lozinski, Maciej AU - Czarniecka, Urszula AU - Lewinska, Lena TI - The intramontane Orava Basin - evidence of large-scale Miocene to Quaternary sinistral wrenching in the Alpine-Carpathian-Pannonian area JF - ACTA GEOLOGICA POLONICA J2 - ACTA GEOL POL VL - 69 PY - 2019 IS - 3 SP - 339 EP - 386 PG - 48 SN - 0001-5709 DO - 10.24425/agp.2019.126449 UR - https://m2.mtmt.hu/api/publication/30797506 ID - 30797506 N1 - Faculty of Geology, University of Warsaw, Żwirki i Wigury 93, Warsaw, 02-089, Poland Department of Geosciences, University of Oslo, P.O. Box 1047 Blindern, Oslo, 0316, Norway Cited By :9 Export Date: 1 July 2022 Correspondence Address: Ludwiniak, M.; Faculty of Geology, Żwirki i Wigury 93, Poland; email: Miroslaw.Ludwiniak@uw.edu.pl LA - English DB - MTMT ER - TY - JOUR AU - Lukoczki, Georgina AU - Haas, János AU - Gregg, JM AU - Machel, HG AU - Kele, Sándor AU - John, CM TI - Multi-phase dolomitization and recrystallization of Middle Triassic shallow marine–peritidal carbonates from the Mecsek Mts. (SW Hungary), as inferred from petrography, carbon, oxygen, strontium and clumped isotope data JF - MARINE AND PETROLEUM GEOLOGY J2 - MAR PETROL GEOL VL - 101 PY - 2019 SP - 440 EP - 458 PG - 19 SN - 0264-8172 DO - 10.1016/j.marpetgeo.2018.12.004 UR - https://m2.mtmt.hu/api/publication/30342399 ID - 30342399 N1 - Funding Agency and Grant Number: American Association of Petroleum Geologists; Geological Society of America Graduate Student Research Grant Program; International Association of Sedimentologists; Hungarian Scientific Research FundOrszagos Tudomanyos Kutatasi Alapprogramok (OTKA) [OTKA K124313]; National Research, Development and Innovation Office (NKFIH) [KH 125584] Funding text: This work was supported by the American Association of Petroleum Geologists Grants-in-Aid Program, the Geological Society of America Graduate Student Research Grant Program, the International Association of Sedimentologists Post-Graduate Grant Scheme, and the Hungarian Scientific Research Fund (OTKA K124313). SK was supported by the National Research, Development and Innovation Office (NKFIH, KH 125584). The authors are indebted to Tames Budai and Gyula Konrad for their continued help and support, and to Mecsekerc Ltd. for providing access to the VP-2 drill cores. The comments and suggestions of Alessandro Iannace and an anonymous reviewer are greatly appreciated. This is an Oklahoma State University Boone Pickens School of Geology contribution #2018-93. LA - English DB - MTMT ER - TY - JOUR AU - Mádlné Szőnyi, Judit AU - Czauner, Brigitta AU - Iván, Veronika AU - Tóth, Ádám AU - Simon, Szilvia AU - Erőss, Anita AU - Kovácsné Bodor, Petra AU - Trásy-Havril, Tímea AU - Boncz, László AU - Sőreg, Viktor TI - Confined carbonates–Regional scale hydraulic interaction or isolation? JF - MARINE AND PETROLEUM GEOLOGY J2 - MAR PETROL GEOL VL - 107 PY - 2019 SP - 591 EP - 612 PG - 22 SN - 0264-8172 DO - 10.1016/j.marpetgeo.2017.06.006 UR - https://m2.mtmt.hu/api/publication/3240055 ID - 3240055 N1 - József and Erzsébet Tóth Endowed Hydrogeology Chair, Department of Physical and Applied Geology, Faculty of Science, Eötvös Loránd University, 1/C Pázmány P. stny. Budapest-1117, Hungary MOL Hungarian Oil and Gas Public Limited Company, 18 Oktober 23. St. Budapest-1117, Hungary Cited By :10 Export Date: 1 July 2022 Correspondence Address: Mádl-Szőnyi, J.; József and Erzsébet Tóth Endowed Hydrogeology Chair, 1/C Pázmány P. stny. Budapest-1117, Hungary; email: szjudit@ludens.elte.hu LA - English DB - MTMT ER - TY - JOUR AU - Mészáros, Előd AU - Raucsikné Varga, Andrea Beáta AU - Raucsik, Béla AU - Benkó, Zsolt AU - Heincz, Adrián László AU - Hauzenberger, CA TI - Provenance and Variscan low-grade regional metamorphism recorded in slates from the basement of the (SW Hungary) JF - INTERNATIONAL JOURNAL OF EARTH SCIENCES J2 - INT J EARTH SCI VL - 108 PY - 2019 IS - 5 SP - 1571 EP - 1593 PG - 23 SN - 1437-3254 DO - 10.1007/s00531-019-01720-y UR - https://m2.mtmt.hu/api/publication/30658244 ID - 30658244 N1 - Funding Agency and Grant Number: University of Szeged (SZTE); Department of Mineralogy, Geochemistry and Petrology; Bolyai Research Scholarship of the Hungarian Academy of SciencesHungarian Academy of Sciences [BO/266/18, BO/442/16]; European UnionEuropean Commission; State of Hungary; European Regional Development FundEuropean Commission [GINOP-2.3.2.-15-2016-00009]; New National Excellence Program of the Ministry of Human Capacities (Hungary) [UNKP-17-4]; Hungarian Scientific Research Found project (Hungary) [PD 83511] Funding text: Open access funding provided by University of Szeged (SZTE). We acknowledge Laurence Warr (University of Greifswald) for the CIS standards and Elemer Pal-Molnar (University of Szeged) for support of the "Vulcano' Petrology and Geochemistry Research Group, and Felix Schubert for the helpful conversations. We thank Zoltan Mathe (Mecsekerc Ltd.) and Gyorgy Szakmany (Eotvos Lorand University) and Gyongyi Lelkesne Felvari (Hungarian Academy of Sciences) for the studied samples. We thank Tivadar M. Toth for the support of the Department of Mineralogy, Geochemistry and Petrology. The KAr studies were supported by the Bolyai Research Scholarship of the Hungarian Academy of Sciences(BO/442/16) to Zsolt Benko. The research was supported by the European Union and the State of Hungary, cofinanced by the European Regional Development Fund in the project of GINOP-2.3.2.-15-2016-00009 "ICER'. Geochemical and regional correlation studies were supported by the UNKP-17-4 New National Excellence Program of the Ministry of Human Capacities (Hungary) and the Bolyai Research Scholarship of the Hungarian Academy of Sciences(BO/266/18) to Andrea Varga. Some parts of this research was financed by the Hungarian Scientific Research Found project PD 83511 (Hungary) to Andrea Varga. We would like to thank the anonymous reviewers and Ingo Braun (topic editor) for their suggestions and comments that improve our manuscript. LA - English DB - MTMT ER - TY - JOUR AU - Patkó, Levente AU - Liptai, Nóra AU - Kovács, István János AU - Aradi, László Előd AU - Xia, Q.-K. AU - Ingrin, J. AU - Mihály, Judith AU - O'Reilly, S.Y. AU - Griffin, W.L. AU - Wesztergom, Viktor AU - Szabó, Csaba TI - Extremely low structural hydroxyl contents in upper mantle xenoliths from the Nógrád-Gömör Volcanic Field (northern Pannonian Basin): Geodynamic implications and the role of post-eruptive re-equilibration JF - CHEMICAL GEOLOGY J2 - CHEM GEOL VL - 507 PY - 2019 IS - 5 SP - 23 EP - 41 PG - 19 SN - 0009-2541 DO - 10.1016/j.chemgeo.2018.12.017 UR - https://m2.mtmt.hu/api/publication/30642272 ID - 30642272 N1 - Export Date: 23 April 2019 Lithosphere Fluid Research Lab, Institute of Geography and Earth Sciences, Eötvös University, Budapest, Hungary Australian Research Council Centre of Excellence for Core to Crust Fluid Systems (CCFS) and GEMOC, Department of Earth and Planetary Sciences, Macquarie University, Sydney, Australia MTA CSFK Lendület Pannon LitH 2 Oscope Research Group , Geodetic and Geophysical Institute, Research Centre for Astronomy and Earth Sciences, Hungarian Academy of Sciences, Sopron, Hungary School of Earth Sciences, Zhejiang University, Hangzhou, China Univ. Lille, CNRS, INRA, ENSCL, UMR 8207, UMET, Unité Matériaux et Transformations, Lille, F 59 000, France Research Centre for Natural Sciences, Hungarian Academy of Sciences, Budapest, Hungary Cited By :2 Export Date: 27 November 2019 Correspondence Address: Kovács, I.J.; MTA CSFK Lendület Pannon LitH 2 Oscope Research Group, Geodetic and Geophysical Institute, Research Centre for Astronomy and Earth Sciences, Hungarian Academy of SciencesHungary; email: kovacs.istvan.janos@csfk.mta.hu LA - English DB - MTMT ER - TY - JOUR AU - Petrik, Attila AU - Fodor, László AU - Bereczki, László AU - Klembala, Zs AU - Haranginé Lukács, Réka AU - Baranyi, Viktória AU - Beke, Barbara AU - Harangi, Szabolcs TI - Variation in style of magmatism and emplacement mechanism induced by changes in basin environments and stress fields (Pannonian Basin, Central Europe) JF - BASIN RESEARCH J2 - BASIN RES VL - 31 PY - 2019 IS - 2 SP - 380 EP - 404 PG - 25 SN - 0950-091X DO - 10.1111/bre.12326 UR - https://m2.mtmt.hu/api/publication/30321155 ID - 30321155 LA - English DB - MTMT ER - TY - JOUR AU - Schmid, SM. AU - Fügenschuh, B AU - Kounov, A AU - Matenco, L AU - Nievergelt, P AU - Oberhänsli, R AU - Pleuger, J AU - Schefer, S AU - Schuster, R AU - Tomljenović, B AU - Ustaszewski, K AU - van Hinsbergen, DJJ. TI - Tectonic units of the Alpine collision zone between Eastern Alps and western Turkey JF - GONDWANA RESEARCH J2 - GONDWANA RES VL - 78 PY - 2019 SP - 308 EP - 374 PG - 67 SN - 1342-937X DO - 10.1016/j.gr.2019.07.005 UR - https://m2.mtmt.hu/api/publication/30802650 ID - 30802650 N1 - Funding Agency and Grant Number: Swiss National Science FoundationSwiss National Science Foundation (SNSF) [200021-101882/1, Pl-534/3-1]; Deutsche ForschungsgemeinschaftGerman Research Foundation (DFG) Funding text: This compilation profited from intense interactions with numerous colleagues and friends who generously shared their profound knowledge with us. Amongst all of them, too numerous to mention them all of them, we specifically would like to mention Philipp Balling (Jena), Romain Bousquet (Kiel), Mark Handy (Berlin), Daniel Bernoulli (Basel), Albrecht von Quadt (Zurich), Dusan Plasienka (Bratislava), Janos Haas, Lazlo Fodor, Laszlo Csontos, Sandor Kovacsy and Frank Horvathy (Budapest), Marko Vrabec (Ljubljana), Jakob Pamicy and Bosko Lugovicy (Zagreb), Hazim Hrvatovic (Sarajevo), Milan Sudar, Natasa Gerzina, Nevenka Deric, Vladica Cvetkovic, Dejan Prelevic, Marinko Toljic and Stevan Karamatay (Belgrade), Neven Georgiev (Sofia), Nikola Dumurdjanov (Skopje), Kujtim Onuzi (Tirana), Tudor Berza, Antoneta Seghedi and Mircea Sandulescuy (Bucharest), Aral Okay (Istanbul) and Osman Parlak (Adana). We acknowledge financial support by the Swiss National Science Foundation grant Nr. 200021-101882/1 (S.M. Schmid) and grant Nr. Pl-534/3-1 by the Deutsche Forschungsgemeinschaft (J. Pleuger). Finally we thank Aral Okay and an anonymous reviewer for their reviews that helped to substantially improve this contribution. Institute of Geophysics ETHZ, ETH-Zentrum, Zürich, 8092, Switzerland Department of Geology, Universität Innsbruck, Innsbruck, Austria Department of Environmental Sciences, Universität Basel, Basel, Switzerland Faculty of Geosciences, Universiteit Utrecht, Netherlands Institute of Geochemistry and Petrology ETHZ, Zürich, Switzerland Department of Earth and Environmental Sciences, University of Potsdam, Germany Institute of Geological Sciences, Freie Universität Berlin, Germany Geologische Bundesanstalt, Wien, Austria Faculty of Mining, Geology and Petroleum Engineering, University of Zagreb, Croatia Institute of Geological Sciences, University Jena, Germany Cited By :24 Export Date: 8 January 2021 Correspondence Address: Schmid, S.M.; Institute of Geophysics ETHZ, ETH-Zentrum, Switzerland; email: stefan.schmid@unibas.ch Funding details: Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung, SNF Funding text 1: This compilation profited from intense interactions with numerous colleagues and friends who generously shared their profound knowledge with us. Amongst all of them, too numerous to mention them all of them, we specifically would like to mention Philipp Balling (Jena), Romain Bousquet (Kiel), Mark Handy (Berlin), Daniel Bernoulli (Basel), Albrecht von Quadt (Zürich), Dušan Plašienka (Bratislava), Janos Haas, Lazlo Fodor, Laszlo Csontos, Sándor Kovács† and Frank Horváth† (Budapest), Marko Vrabec (Ljubljana), Jakob Pamić† and Boško Lugović† (Zagreb), Hazim Hrvatović (Sarajevo), Milan Sudar, Nataša Gerzina, Nevenka Đerić, Vladica Cvetković, Dejan Prelević, Marinko Toljić and Stevan Karamata† (Belgrade), Neven Georgiev (Sofia), Nikola Dumurdjanov (Skopje), Kujtim Onuzi (Tirana), Tudor Berza, Antoneta Seghedi and Mircea Săndulescu† (Bucharest), Aral Okay (Istanbul) and Osman Parlak (Adana). We acknowledge financial support by the Swiss National Science Foundation grant Nr. 200021-101882/1 (S.M. Schmid) and grant Nr. Pl-534/3-1 by the Deutsche Forschungsgemeinschaft (J. Pleuger). Finally we thank Aral Okay and an anonymous reviewer for their reviews that helped to substantially improve this contribution. Funding text 2: Bernhard Fügenschuh (PhD, ETH Zürich, 1995) is full professor of structural geology and geodynamics and since 2016 vice rector at Innsbruck University, Austria. He was a post-doctoral fellow at Basel University in the group of Stefan Schmid. His dominantly field-based research focuses mainly on the evolution of the Alps, Carpathians and Dinarides and their southeastward extensions. Methodologically, he used low-temperature thermochronology together with microstructural analyses to aid field observations and interpretations. Research projects were sponsored by the ETH-fund, the Swiss National Science foundation (SNF) and the Austrian Science Fund (FWF). He authored and co-authored more than 50 publications in peer-reviewed journals and is vice-president of the German Geological Society (DGGV). Funding Agency and Grant Number: Swiss National Science FoundationSwiss National Science Foundation (SNSF)European Commission [200021-101882/1, Pl-534/3-1]; Deutsche ForschungsgemeinschaftGerman Research Foundation (DFG) Funding text: This compilation profited from intense interactions with numerous colleagues and friends who generously shared their profound knowledge with us. Amongst all of them, too numerous to mention them all of them, we specifically would like to mention Philipp Balling (Jena), Romain Bousquet (Kiel), Mark Handy (Berlin), Daniel Bernoulli (Basel), Albrecht von Quadt (Zurich), Dusan Plasienka (Bratislava), Janos Haas, Lazlo Fodor, Laszlo Csontos, Sandor Kovacsy and Frank Horvathy (Budapest), Marko Vrabec (Ljubljana), Jakob Pamicy and Bosko Lugovicy (Zagreb), Hazim Hrvatovic (Sarajevo), Milan Sudar, Natasa Gerzina, Nevenka Deric, Vladica Cvetkovic, Dejan Prelevic, Marinko Toljic and Stevan Karamatay (Belgrade), Neven Georgiev (Sofia), Nikola Dumurdjanov (Skopje), Kujtim Onuzi (Tirana), Tudor Berza, Antoneta Seghedi and Mircea Sandulescuy (Bucharest), Aral Okay (Istanbul) and Osman Parlak (Adana). We acknowledge financial support by the Swiss National Science Foundation grant Nr. 200021-101882/1 (S.M. Schmid) and grant Nr. Pl-534/3-1 by the Deutsche Forschungsgemeinschaft (J. Pleuger). Finally we thank Aral Okay and an anonymous reviewer for their reviews that helped to substantially improve this contribution. LA - English DB - MTMT ER - TY - JOUR AU - Šimonová, Barbora AU - Zeyen, Hermann AU - Bielik, Miroslav TI - Continental lithospheric structure from the East European Craton to the Pannonian Basin based on integrated geophysical modelling JF - TECTONOPHYSICS J2 - TECTONOPHYSICS VL - 750 PY - 2019 SP - 289 EP - 300 PG - 12 SN - 0040-1951 DO - 10.1016/j.tecto.2018.12.003 UR - https://m2.mtmt.hu/api/publication/30388038 ID - 30388038 N1 - Cited By :5 Export Date: 1 July 2022 Correspondence Address: Zeyen, H.; GEOPS, France; email: hermann.zeyen@u-psud.fr LA - English DB - MTMT ER - TY - JOUR AU - Garaguly, István AU - Raucsikné Varga, Andrea Beáta AU - Raucsik, Béla AU - Schubert, Félix AU - Czuppon, György AU - Frei, R TI - Pervasive early diagenetic dolomitization, subsequent hydrothermal alteration, and late stage hydrocarbon accumulation in a Middle Triassic carbonate sequence (Szeged Basin, SE Hungary) JF - MARINE AND PETROLEUM GEOLOGY J2 - MAR PETROL GEOL VL - 98 PY - 2018 SP - 270 EP - 290 PG - 21 SN - 0264-8172 DO - 10.1016/j.marpetgeo.2018.07.024 UR - https://m2.mtmt.hu/api/publication/3399845 ID - 3399845 N1 - Funding Agency and Grant Number: National Research, Development and Innovation Fund of Hungary [K 108375] Funding text: This research was supported by the National Research, Development and Innovation Fund of Hungary (project no. K 108375). The authors would like to thank MOL Plc for providing the core material that were essential for this research. We would like to thank Dr. Fadi H. Nader and the anonymous referee for their suggestions and comments that improve our manuscript, as well as Associated Editor Dr. Ihsan Al-Aasm for the editorial work. Department of Mineralogy, Geochemistry and Petrology, University of Szeged, Egyetem utca 2-6, Szeged, 6702, Hungary Institute for Geological and Geochemical Research, Research Centre for Astronomy and Earth Sciences, Hungarian Academy of Sciences, Budaörsi út 45, Budapest, H-1112, Hungary Department of Geosciences and Natural Resource Management, University of Copenhagen, ØsterVoldgade10, Copenhagen, 1350, Denmark Nordic Center for Earth Evolution (NordCEE), Copenhagen, Denmark Cited By :15 Export Date: 12 September 2021 Correspondence Address: Garaguly, I.; Department of Mineralogy, Egyetem utca 2-6, Hungary; email: garagulyistvan@gmail.com Funding text 1: This research was supported by the National Research, Development and Innovation Fund of Hungary (project no. K 108375 ). The authors would like to thank MOL Plc for providing the core material that were essential for this research. We would like to thank Dr. Fadi H. Nader and the anonymous referee for their suggestions and comments that improve our manuscript, as well as Associated Editor Dr. Ihsan Al-Aasm for the editorial work. LA - English DB - MTMT ER - TY - JOUR AU - Godova, Dominika AU - Bielik, Miroslav AU - Simonova, Barbora TI - The deepest Moho in the Western Carpathians and its respective crustal density model (CEL12 section) JF - CONTRIBUTIONS TO GEOPHYSICS AND GEODESY J2 - CONTRIB GEOPHYS GEODES VL - 48 PY - 2018 IS - 3 SP - 255 EP - 269 PG - 15 SN - 1335-2806 DO - 10.2478/congeo-2018-0011 UR - https://m2.mtmt.hu/api/publication/30430761 ID - 30430761 N1 - Department of Applied and Environmental Geophysics, Faculty of Natural Sciences, Comenius University, Mlynská dolina, Ilkovičova 6, Bratislava, 842 48, Slovakia Earth Science Institute, Slovak Academy of Sciences, Dúbravská cesta 9, P. O. Box 106, Bratislava, 840 05, Slovakia Cited By :1 Export Date: 1 July 2022 LA - English DB - MTMT ER - TY - JOUR AU - Horvat, M. AU - Klötzli, U. AU - Jamičić, D. AU - Buda, György AU - Klötzli, E. AU - Hauzenberger, C. TI - Geochronology of granitoids from Psunj and Papuk Mts., Croatia JF - GEOCHRONOMETRIA J2 - GEOCHRONOMETRIA VL - 45 PY - 2018 IS - 1 SP - 198 EP - 210 PG - 13 SN - 1733-8387 DO - 10.1515/geochr-2015-0099 UR - https://m2.mtmt.hu/api/publication/30321138 ID - 30321138 N1 - \n Croatian Geological Survey, Department of Geology, Sachsova 2, Zagreb, 10000, Croatia \n University of Vienna, Department of Lithospheric Research, Althanstraße 14, Vienna, A-1090, Austria \n Svetojanska 21, Zagreb, 10000, Croatia \n Eötvös Lóránd University, Institute of Geology, Department of Mineralogy, Pazmany Peter setany 1/c, Budapest, H-1117, Hungary \n Karl-Franzens-University, Department of Earth Sciences, Universitätsplatz 2, Graz, 8010, Austria \n Export Date: 19 November 2018 \n Correspondence Address: Horvat, M.; Croatian Geological Survey, Department of Geology, Sachsova 2, Croatia; email: mhorvat@hgi-cgs.hr Funding Agency and Grant Number: Ministry of Science and Education of the Republic of Croatia; OTKA (Hungarian National Research Fund) [K 67787]; Hungarian Ministry of Education\n Funding text: This work was financed by Ministry of Science and Education of the Republic of Croatia, and supported by OTKA (Hungarian National Research Fund project no. K 67787). The study was carried out partly at the Department of Mineralogy, Eotvos Lorand University, Budapest, and was supported by the Hungarian Ministry of Education through the Ph.D. scholarship of the first author. The study was also carried out at the Department of Geology of the Croatian Geological Survey, as well as at the Department of Lithospheric Research, the University of Vienna, the Department of Earth Sciences, Karl-Franzens-Universitat Graz and the Institute of Applied Geosciences, the Graz Technical University. The authors are very grateful to Livia Rudnyanszky (Department of Mineralogy, Eotvos Lorand University) for zircon separation and Franz Biedermann (Department of Lithospheric Research, University of Vienna) for the preparation of BSE/CL images. The authors would also like to acknowledge Mirko Belak (Department of Geology, Croatian Geological Survey) for useful discussion. Special thanks go to Christian Auer (Geological Survey of Austria, Vienna) for scanning electron microscopy facilities. The authors would like to thank to three anonymous reviewers for their constructive comments, objections and suggestions which have contributed in the reorganization and improvement of the manuscript.\n Funding Agency and Grant Number: Ministry of Science and Education of the Republic of Croatia; OTKA (Hungarian National Research Fund)Orszagos Tudomanyos Kutatasi Alapprogramok (OTKA) [K 67787]; Hungarian Ministry of Education Funding text: This work was financed by Ministry of Science and Education of the Republic of Croatia, and supported by OTKA (Hungarian National Research Fund project no. K 67787). The study was carried out partly at the Department of Mineralogy, Eotvos Lorand University, Budapest, and was supported by the Hungarian Ministry of Education through the Ph.D. scholarship of the first author. The study was also carried out at the Department of Geology of the Croatian Geological Survey, as well as at the Department of Lithospheric Research, the University of Vienna, the Department of Earth Sciences, Karl-Franzens-Universitat Graz and the Institute of Applied Geosciences, the Graz Technical University. The authors are very grateful to Livia Rudnyanszky (Department of Mineralogy, Eotvos Lorand University) for zircon separation and Franz Biedermann (Department of Lithospheric Research, University of Vienna) for the preparation of BSE/CL images. The authors would also like to acknowledge Mirko Belak (Department of Geology, Croatian Geological Survey) for useful discussion. Special thanks go to Christian Auer (Geological Survey of Austria, Vienna) for scanning electron microscopy facilities. The authors would like to thank to three anonymous reviewers for their constructive comments, objections and suggestions which have contributed in the reorganization and improvement of the manuscript. AB - Detailed cathodoluminescence (CL) and back scattered electron (BSE) imaging of zircon crystals, coupled with in-situ U-Pb zircon dating by Laser Ablation Multi-Collector Inductively Coupled Plasma Mass Spectrometry (LA-MC-ICP-MS) were used to develop new insights into the evolution of a monzogranite from Omanovac Quarry (Psunj Mt.), and of monzogranites from Sandrovac Quarry and Kiseljevac Creek (Papuk Mt.), both located in the Slavonian Mountains (Croatia). U-Pb isotopic data yielded a concordia age of 380 +/- 4 Ma for the monzogranite from Omanovac Quarry, and 382 +/- 2 Ma and 383 +/- 5 Ma for monzogranites from Sandrovac Quarry and Kiseljevac Creek. The results suggest Late Devonian magmatic activity. LA - English DB - MTMT ER - TY - JOUR AU - Ivancic, Kristina AU - Trajanova, Mirka AU - Coric, Stjepan AU - Rozic, Bostjan AU - Smuc, Andrej TI - Miocene paleogeography and biostratigraphy of the Slovenj Gradec Basin: a marine corridor between the Mediterranean and Central Paratethys JF - GEOLOGICA CARPATHICA J2 - GEOL CARPATH VL - 69 PY - 2018 IS - 6 SP - 528 EP - 544 PG - 17 SN - 1335-0552 DO - 10.1515/geoca-2018-0031 UR - https://m2.mtmt.hu/api/publication/30432320 ID - 30432320 N1 - Geological Survey of Slovenia, Dimičeva ulica 14, Ljubljana, 1000, Slovenia Geologische Bundesanstalt, Neulinggasse 38, Vienna, 1030, Austria University of Ljubljana, Faculty of Natural Sciences and Engineering, Department of Geology, Privoz 11, Ljubljana, 1000, Slovenia Cited By :10 Export Date: 1 July 2022 Correspondence Address: Ivančič, K.; Geological Survey of Slovenia, Dimičeva ulica 14, Slovenia; email: kristina.ivancic@geo-zs.si LA - English DB - MTMT ER - TY - JOUR AU - Kopotowska, Agnieszka TI - Ultrasonic constraint of the microfracture anisotropy of flysch rocks from the Podhale Synclinorium (Poland) JF - INTERNATIONAL JOURNAL OF EARTH SCIENCES J2 - INT J EARTH SCI VL - 107 PY - 2018 IS - 6 SP - 1941 EP - 1953 PG - 13 SN - 1437-3254 DO - 10.1007/s00531-017-1579-1 UR - https://m2.mtmt.hu/api/publication/30479664 ID - 30479664 N1 - Cited By :2 Export Date: 1 July 2022 CODEN: IJESF Correspondence Address: Kłopotowska, A.; Faculty of Geology, Poland; email: a.klopotowska@uw.edu.pl AB - This paper attempts to show the relationship between joints observed in flysch formations in the field and microfracture fabrics invisible to the naked eye in hand specimens. Ultrasonic measurements demonstrate that the intensity and orientations of domains "memorised" by rock specimens are associated with the historical stresses within the rock mass rather than the rock lamination. The spatial orientations of these microfractures have been measured, and their dynamic-elastic properties have been found to correlate with the orientation of macroscopic joint sets measured in the field. The elastic properties measured vary because of sedimentary diagenetic processes that occured during the tectonic deformations of these flysch rocks in the Podhale Synclinorium of Poland. The structural discontinuities detected by ultrasonic measurements can be perceived as an incipient phase of the macroscopic joints already visible in the field and are attributed to the in situ residual tectonic stresses. Such historical stresses impart a hidden mechanical anisotropy to the entire flysch sequence. The microfractures will develop into macroscopic joints during future relaxation of the exposed rock mass. Understanding the nature and orientation of the invisible microfracture anisotropy that will become macroscopic in the future is vital for the safe and efficient engineering of any rock mass. LA - English DB - MTMT ER - TY - JOUR AU - Kovac, M AU - Rybar, S AU - Halasova, E AU - Hudackova, N AU - Sarinova, K AU - Sujan, M AU - Baranyi, Viktória AU - Kovacova, M AU - Ruman, A AU - Kluciar, T AU - Zlinska, A TI - Changes in Cenozoic depositional environment and sediment provenance in the Danube Basin JF - BASIN RESEARCH J2 - BASIN RES VL - 30 PY - 2018 IS - 1 SP - 97 EP - 131 PG - 35 SN - 0950-091X DO - 10.1111/bre.12244 UR - https://m2.mtmt.hu/api/publication/27587223 ID - 27587223 N1 - Department of Geology and Paleontology, Faculty of Natural Sciences, Comenius University in Bratislava, Bratislava, Slovakia Department of Mineralogy and Petrology, Faculty of Natural Sciences, Comenius University in Bratislava, Bratislava, Slovakia Department of Geosciences, University of Oslo, Oslo, Norway State Geological Institute of Dionýz Štúr, Bratislava, Slovakia Cited By :9 Export Date: 27 November 2019 Correspondence Address: Kováč, M.; Department of Geology and Paleontology, Faculty of Natural Sciences, Comenius University in BratislavaSlovakia; email: kovacm@fns.uniba.sk LA - English DB - MTMT ER - TY - JOUR AU - Kovac, M AU - Márton Péterné Szalay, Emőke AU - Kluciar, T AU - Vojtko, R TI - Miocene basin opening in relation to the north-eastward tectonic extrusion of the ALCAPA Mega-Unit JF - GEOLOGICA CARPATHICA J2 - GEOL CARPATH VL - 69 PY - 2018 IS - 3 SP - 254 EP - 263 PG - 10 SN - 1335-0552 DO - 10.1515/geoca-2018-0015 UR - https://m2.mtmt.hu/api/publication/3391954 ID - 3391954 N1 - OA gold Department of Geology and Palaeontology, Faculty of Natural Sciences, Comenius University in Bratislava, Mlynská dolina, Ilkovičova 6, S-Bratislava, 842 15, El Salvador Mining and Geological Survey of Hungary, Palaeomagnetic Laboratory, Columbus 17-23, Budapest, H-1145, Hungary Export Date: 10 January 2019 Correspondence Address: Kováč, M.; Department of Geology and Palaeontology, Faculty of Natural Sciences, Comenius University in Bratislava, Mlynská dolina, Ilkovičova 6, El Salvador; email: kovacm@uniba.sk Department of Geology and Palaeontology, Faculty of Natural Sciences, Comenius University in Bratislava, Mlynská dolina, Ilkovičova 6, S-Bratislava, 842 15, El Salvador Mining and Geological Survey of Hungary, Palaeomagnetic Laboratory, Columbus 17-23, Budapest, H-1145, Hungary Export Date: 27 November 2019 Correspondence Address: Kováč, M.; Department of Geology and Palaeontology, Faculty of Natural Sciences, Comenius University in Bratislava, Mlynská dolina, Ilkovičova 6, El Salvador; email: kovacm@uniba.sk AB - The opening and evolution of the Western Carpathians Miocene basins was closely related to the north-eastward tectonic extrusion of the ALCAPA Mega-Unit lithosphere caused by the final stage of collision of the Eastern Alpine-Western Carpathian orogenic system with the European Platform and Alpine convergence with the Adria plate. The roll back effect of the oceanic or thinned continental crust of the Magura-Krosno realms, subduction below the front of the Carpathians in the north-east, east and relative plate velocities led to gradual stretching of the overriding micro-plates (defined as the ALCAPA and Tisza Dacia Mega-Unit). Diverse movement trajectories of the ALCAPA crustal wedge individual segments (Eastern Alps, Western Carpathians, and Northern Pannonian domain) were accompanied by several counter-clockwise rotational phases. Beside the interpreted Early Miocene "en-block" counter-clockwise rotation, most of the rotations in the Central Western Carpathians were caused by "domino-effect tectonics" inside strike-slip zones and took part in the basin opening, which was in most cases followed by rapid subsidence. LA - English DB - MTMT ER - TY - JOUR AU - Lee, Eun Young AU - Wagreich, Michael TI - Basin modelling with a MATLAB-based program, BasinVis 2.0: A case study on the southern Vienna Basin, Austria JF - JOURNAL OF THE GEOLOGICAL SOCIETY OF KOREA J2 - J GEO SOC KOREA VL - 54 PY - 2018 IS - 6 SP - 615 EP - 630 PG - 16 SN - 0435-4036 DO - 10.14770/jgsk.2018.54.6.615 UR - https://m2.mtmt.hu/api/publication/30479651 ID - 30479651 AB - Basin analysis is a research field to understand the formation and evolution of sedimentary basins. This task requires various geoscientific datasets as well as numerical and graphical modelling techniques to synthesize results dimensionally in time and space. For basin analysis and modelling in a comprehensive workflow, BasinVis 1.0 was released as a MATLAB-based program in 2016, and recently the software has been extended to BasinVis 2.0, with new functions and revised user-interface. As a case study, this work analyses the southern Vienna Basin and visualizes the sedimentation setting and subsidence evolution to introduce the basin modelling functions of BasinVis 2.0. This is a preliminary study for a basin-scale modelling of the Vienna Basin, together with our previous studies using BasinVis 1.0. In the study area, during the late Early Miocene, sedimentation and subsidence are significant along strike-slip and en-echelon listric normal faults. From the Middle Miocene onwards, however, subsidence decreases abruptly over the area and this situation continues until the Late Miocene. This is related to the development of the pull-apart system and corresponds to the episodic tectonic subsidence in strike-slip basins. The subsidence of the Middle Miocene is confined mainly to areas along the strike-slip faults, while, from the late Middle Miocene, the depocenter shifts to a depression along the N-S trending listric normal faults. This corresponds to the regional paleostress regime transitioning from NE-SW trending transtension to E-W trending extension. This study applies various functions and techniques to this case study, and the modelled results demonstrate that BasinVis 2.0 is effective and applicable to the basin modelling. LA - English DB - MTMT ER - TY - JOUR AU - Haranginé Lukács, Réka AU - Harangi, Szabolcs AU - Guillong, M AU - Bachmann, O AU - Fodor, László AU - Buret, Y AU - Dunkl, István AU - Sliwinski, J AU - von Quadt, A AU - Peytcheva, I AU - Zimmerer, M TI - Early to Mid-Miocene syn-extensional massive silicic volcanism in the Pannonian Basin (East-Central Europe): Eruption chronology, correlation potential and geodynamic implications JF - EARTH-SCIENCE REVIEWS J2 - EARTH-SCI REV VL - 179 PY - 2018 SP - 1 EP - 19 PG - 19 SN - 0012-8252 DO - 10.1016/j.earscirev.2018.02.005 UR - https://m2.mtmt.hu/api/publication/3339119 ID - 3339119 AB - Formation and evolution of the Pannonian Basin as part of the Mediterranean region was accompanied by eruptions of compositionally diverse magmas during the Neogene to Quaternary. The long-lasting magmatic activity began with some of the most voluminous silicic eruptions in Europe for the last 20 Myr. This paper describes the eruption chronology of this volcanic activity using new, high-quality zircon U-Pb dates, and provides the first estimates on the volume and areal distribution of the volcanic products, characterizes the magma composition and discusses the silicic magmatism in a region, where the continental lithosphere underwent significant extension. A thorough zircon geochronological study was conducted on samples collected from ignimbrites and pyroclastic fall deposits exposed in the Bükkalja Volcanic Field. In-situ LA-ICP-MS analysis on zircon grains provided a fast, cheap and accurate method for such detailed geochronological work, where the volcanic products occur in scattered outcrops that often have poor stratigraphic constraints. The interpreted eruption ages were determined from the youngest zircon age population within the samples and this methodology was validated by new single zircon CA-ID-TIMS dates and sanidine Ar-Ar ages. The volcanism covers about 4 Myrs, from 18.2 Ma to 14.4 Ma and involved at least eight eruptive phases. Within this, four large eruption events were recognized at 14.358 ± 0.015 Ma (Harsány ignimbrite), 14.880 ± 0.014 Ma (Demjén ignimbrite), 16.816 ± 0.059 Ma (Bogács unit) and 17.055 ± 0.024 Ma (Mangó ignimbrite), which are found in areas across the Pannonian Basin and elsewhere in central Europe. Considering all the potential sources of silicic ash found in the Paratethys sub-basins around the Pannonian Basin and along the northern Alps and in central Italy, we suggest that they were probably derived almost exclusively from the Pannonian Basin as shown by zircon U-Pb dates presented in this paper and published comparable age data from several localities. The new eruption ages considerably refine the Early to Mid-Miocene chronostratigraphy of the Pannonian basin, where the extensive volcanoclastic horizons are used as important marker layers. The cumulative volume of the volcanic material formed during this 4 Myr long silicic volcanism is estimated to be >4000 km3, consistent with a significant ignimbrite flare-up event. Zircon crystallization ages indicate magma intrusions and formations of magma reservoirs in the continental crust for prolonged period, likely >1 Myr prior to the onset of the silicic volcanism accompanied with sporadic andesitic to dacitic volcanic activities. Mafic magmas were formed by melting of the thinned lithospheric mantle metasomatized previously by subduction-related fluids and emplaced at the crust-mantle boundary. They evolved further by assimilation and fractional crystallization to generate silicic magmas, which ascended into the pre-warmed upper crust and formed extended magma storage regions. Zircon Hf isotope and bulk rock Sr-Nd isotopic data indicate a sharp decrease of crustal and/or increase of asthenospheric mantle input after 16.2 Ma, suggesting that by this time the crust, and the lithospheric mantle was considerably thinned. This magmatism appears to have had a structural relationship to tectonic movements characterized by strike-slip and normal faults within the Mid-Hungarian Shear Zone as well as vertical axis block rotations, when the two microplates were juxtaposed. Our new zircon ages helped to refine the age of two major block-rotation phases associated with faulting. This volcanism shows many similarities with other rift-related silicic volcanic activities such as the Taupo Volcanic Zone (New Zealand) and the Basin and Range Province (USA). LA - English DB - MTMT ER - TY - JOUR AU - Molnár, Kata AU - Harangi, Szabolcs AU - Haranginé Lukács, Réka AU - Dunkl, István AU - Schmitt, AK AU - Kiss, Balázs AU - Garamhegyi, Tamás AU - Seghedi, I TI - The onset of the volcanism in the Ciomadul Volcanic Dome Complex (Eastern Carpathians): Eruption chronology and magma type variation JF - JOURNAL OF VOLCANOLOGY AND GEOTHERMAL RESEARCH J2 - J VOLCANOL GEOTH RES VL - 354 PY - 2018 SP - 39 EP - 56 PG - 18 SN - 0377-0273 DO - 10.1016/j.jvolgeores.2018.01.025 UR - https://m2.mtmt.hu/api/publication/3360352 ID - 3360352 AB - Combined zircon U-Th-Pb and (U-Th)/He dating was applied to refine the eruption chronology of the last 2 Myr for the andesitic and dacitic Pilisca volcano and Ciomadul Volcanic Dome Complex (CVDC), the youngest volcanic area of the Carpathian-Pannonian region, located in the southernmost Harghita, eastern-central Europe. The proposed eruption ages, which are supported also by the youngest zircon crystallization ages, are much younger than the previously determined K/Ar ages. By dating every known eruption center in the CVDC, repose times between eruptive events were also accurately determined. Eruption of the andesite at Murgul Mare (1865 +/- 87 ka) and dacite of the Pilisca volcanic complex (1640 +/- 37 ka) terminated an earlier pulse of volcanic activity within the southernmost Harghita region, west of the Olt valley. This was followed by the onset of the volcanism in the CVDC, which occurred after several 100s kyr of eruptive quiescence. At ca. 1 Ma a significant change in the composition of erupted magma occurred from medium-K calc-alkaline compositions to high-K dacitic (Baba-Laposa dome at 942 +/- 65 ka) and shoshonitic magmas (Malna and Bixad domes: 964 +/- 46 ka and 907 +/- 66 ka, respectively). Noteworthy, eruptions of magmas with distinct chemical compositions occurred within a restricted area, a few km from one another. These oldest lava domes of the CVDC form a NNE-SSW striking tectonic lineament along the Olt valley. Following a brief (ca. 100 kyr) hiatus, extrusion of high-K andesitic magma continued at Dealul Mare (842 +/- 53 ka). After another ca. 200 kyr period of quiescence two high-K dacitic lava domes extruded (Puturosul: 642 +/- 44 ka and Balvanyos: 583 +/- 30 ka). The Turnul Apor lava extrusion occurred after a ca. 200 kyr repose time (at 344 +/- 33 ka), whereas formation of the Haramul Mic lava dome (154 +/- 16 ka) represents the onset of the development of the prominent Ciomadul volcano. The accurate determination of eruption dates shows that the volcanic eruptions were often separated by prolonged (ca. 100 to 200 kyr) quiescence periods. Demonstration of recurrence of volcanism even after such long dormancy has to be considered in assessing volcanic hazards, particularly in seemingly inactive volcanic areas, where no Holocene eruptions occurred. The term of 'volcanoes with Potentially Active Magma Storage' illustrates the potential of volcanic rejuvenation for such long-dormant volcanoes with the existence of melt-bearing crustal magma body. (C) 2018 The Authors. Published by Elsevier B.V. LA - English DB - MTMT ER - TY - JOUR AU - Plašienka, D TI - Continuity and Episodicity in the Early Alpine Tectonic Evolution of the Western Carpathians: How Large-Scale Processes Are Expressed by the Orogenic Architecture and Rock Record Data JF - TECTONICS J2 - TECTONICS VL - 37 PY - 2018 IS - 7 SP - 2029 EP - 2079 PG - 51 SN - 0278-7407 DO - 10.1029/2017TC004779 UR - https://m2.mtmt.hu/api/publication/27642265 ID - 27642265 N1 - Funding Agency and Grant Number: Slovak Research and Development AgencySlovak Research and Development Agency; Grant Agency for Science, Slovakia; [APVV-0212-12]; [APVV-0315-12]; [VEGA 1/0085/17] Funding text: The author is thankful to his numerous collaborators in various problems of the Western Carpathian geology who contributed substantially to the knowledge summarized in the present work. The author's investigations have been maintained by a number of research projects, in the last years by the projects APVV-0212-12, APVV-0315-12, and VEGA 1/0085/17. Financial support from the Slovak Research and Development Agency and from the Grant Agency for Science, Slovakia, is gratefully acknowledged. The paper benefitted from useful suggestions of F. Neubauer, an anonymous reviewer, associate editor E. Willingshofer, and Tectonics editor J. Geissman. Sources of all data presented in the text and figures are listed in references. LA - English DB - MTMT ER - TY - JOUR AU - M. Tóth, Tivadar AU - Schubert, Félix TI - Evolution of the arc-derived orthogneiss recorded in exotic xenoliths of the Koros Complex (Tisza Megaunit, SE Hungary) JF - JOURNAL OF GEOSCIENCES J2 - J GEOSCI VL - 63 PY - 2018 IS - 1 SP - 21 EP - 46 PG - 26 SN - 1802-6222 DO - 10.3190/jgeosci.253 UR - https://m2.mtmt.hu/api/publication/27569302 ID - 27569302 N1 - Funding Agency and Grant Number: Schweizerische NationalfondsSwiss National Science Foundation (SNSF) [21-26579.89] Funding text: The co-operation and discussion with J. Zachar is acknowledged. The electron microprobe laboratory at the University of Bern was sponsored by the Schweizerische Nationalfonds (No.: 21-26579.89). Thorough reviews of Prokop Zavada, Martin Racek and an anonymous reviewer are thanked. P. Hasalova is acknowledged for her editorial work on the manuscript. Cited By :1 Export Date: 11 February 2021 Correspondence Address: Tóth, T.M.; Department of Mineralogy, Egyetem str. 2-6, Hungary; email: mtoth@geo.u-szeged.hu Funding details: Universität Bern, Ub, 21-26579.89 Funding text 1: The co-operation and discussion with J. Zachar is acknowledged. The electron microprobe laboratory at the University of Bern was sponsored by the Schweizerische Nationalfonds (No.: 21-26579.89). Thorough reviews of Prokop Závada, Martin Racek and an anonymous reviewer are thanked. P. Hasalová is acknowledged for her editorial work on the manuscript. Funding text 2: Acknowledgements. The co-operation and discussion with J. Zachar is acknowledged. The electron microprobe laboratory at the University of Bern was sponsored by the Schweizerische Nationalfonds (No.: 21-26579.89). Thorough reviews of Prokop Závada, Martin Racek and an anonymous reviewer are thanked. P. Hasalová is acknowledged for her editorial work on the manuscript. Cited By :1 Export Date: 12 February 2021 Correspondence Address: Tóth, T.M.; Department of Mineralogy, Egyetem str. 2-6, Hungary; email: mtoth@geo.u-szeged.hu Funding details: Universität Bern, Ub, 21-26579.89 Funding text 1: The co-operation and discussion with J. Zachar is acknowledged. The electron microprobe laboratory at the University of Bern was sponsored by the Schweizerische Nationalfonds (No.: 21-26579.89). Thorough reviews of Prokop Závada, Martin Racek and an anonymous reviewer are thanked. P. Hasalová is acknowledged for her editorial work on the manuscript. Funding text 2: Acknowledgements. The co-operation and discussion with J. Zachar is acknowledged. The electron microprobe laboratory at the University of Bern was sponsored by the Schweizerische Nationalfonds (No.: 21-26579.89). Thorough reviews of Prokop Závada, Martin Racek and an anonymous reviewer are thanked. P. Hasalová is acknowledged for her editorial work on the manuscript. Cited By :3 Export Date: 12 September 2021 Correspondence Address: Tóth, T.M.; Department of Mineralogy, Egyetem str. 2-6, Hungary; email: mtoth@geo.u-szeged.hu Funding details: Universität Bern, Ub, 21-26579.89 Funding text 1: The co-operation and discussion with J. Zachar is acknowledged. The electron microprobe laboratory at the University of Bern was sponsored by the Schweizerische Nationalfonds (No.: 21-26579.89). Thorough reviews of Prokop Závada, Martin Racek and an anonymous reviewer are thanked. P. Hasalová is acknowledged for her editorial work on the manuscript. Funding text 2: Acknowledgements. The co-operation and discussion with J. Zachar is acknowledged. The electron microprobe laboratory at the University of Bern was sponsored by the Schweizerische Nationalfonds (No.: 21-26579.89). Thorough reviews of Prokop Závada, Martin Racek and an anonymous reviewer are thanked. P. Hasalová is acknowledged for her editorial work on the manuscript. LA - English DB - MTMT ER - TY - JOUR AU - Bauer, Márton AU - M. Tóth, Tivadar TI - Characterization and DFN modelling of the fracture network in a Mesozoic karst reservoir: Gomba oilfield, Paleogene Basin, Central Hungary JF - JOURNAL OF PETROLEUM GEOLOGY J2 - J PETROL GEOL VL - 40 PY - 2017 IS - 3 SP - 319 EP - 334 PG - 16 SN - 0141-6421 DO - 10.1111/jpg.12678 UR - https://m2.mtmt.hu/api/publication/3331754 ID - 3331754 N1 - : Provider: John Wiley & Sons, Ltd : Content:text/plain; charset="UTF-8" Cited By :12 Export Date: 11 February 2021 CODEN: JPEGD Correspondence Address: Bauer, M.; University of Szeged, Egyetem St 2, Hungary; email: bauer.marton@mfgi.hu Cited By :12 Export Date: 12 February 2021 CODEN: JPEGD Correspondence Address: Bauer, M.; University of Szeged, Egyetem St 2, Hungary; email: bauer.marton@mfgi.hu LA - English DB - MTMT ER - TY - JOUR AU - Brkic, Zeljka TI - The relationship of the geological framework to the Quaternary aquifer system in the Sava River valley (Croatia) JF - GEOLOGIA CROATICA J2 - GEOL CROAT VL - 70 PY - 2017 IS - 3 SP - 201 EP - 213 PG - 13 SN - 1330-030X DO - 10.4154/gc.2017.12 UR - https://m2.mtmt.hu/api/publication/27079576 ID - 27079576 N1 - Cited By :9 Export Date: 1 July 2022 Correspondence Address: Brkić, Ž.; Croatian Geological Survey, Sachsova 2, Croatia; email: zeljka.brkic@hgi-cgs.hr LA - English DB - MTMT ER - TY - JOUR AU - Créon, L AU - Delpech, G AU - Rouchon, V AU - Guyot, F TI - Slab-derived metasomatism in the Carpathian-Pannonian mantle revealed by investigations of mantle xenoliths from the Bakony-Balaton Highland Volcanic Field JF - LITHOS J2 - LITHOS VL - 286-287 PY - 2017 SP - 534 EP - 552 PG - 19 SN - 0024-4937 DO - 10.1016/j.lithos.2017.06.004 UR - https://m2.mtmt.hu/api/publication/26772395 ID - 26772395 N1 - N1 Funding details: IFPEN, IFP Energies Nouvelles N1 Funding text: This project was funded by IFP Energies nouvelles. Thank you to Csaba Szabó for his kind help in the field and in the study of these mantle xenoliths. Herman Ravalojaona is acknowledged for his assistance during sample and thin section preparation. We are grateful to Carole La for her efficient help in LA-ICP-MS analyses of trace elements at LPG Nantes. Michel Fialin and Nicolas Rividi of the centre CAMPARIS at UPMC are acknowledged for their assistance for EPMA analyses. We acknowledge Massimo Coltorti and an anonymous reviewer for their comments which greatly improved the manuscript. Paul Asimow provided a final reading and correction of the manuscript. Összes idézések száma a WoS-ban: 0 IFP Energies nouvelles, 1 & 4 avenue Bois Préau, Rueil-Malmaison Cedex, 92852, France Geosciences Paris Sud Department, Paris Sud University, Bâtiment 504, Orsay Cedex, 91405, France IMPMC, Museum National d'histoire Naturelle, Sorbonne Universités, CNRS, UPMC, IRD, 61 Rue Buffon, Paris, 75005, France Cited By :4 Export Date: 20 April 2021 Correspondence Address: Créon, L.; Universidad Nacional Autónoma de México, Campus Juriquilla, A.P. 1-742, Boulevard Juriquila No. 3001, Mexico; email: lauracreon@gmail.com IFP Energies nouvelles, 1 & 4 avenue Bois Préau, Rueil-Malmaison Cedex, 92852, France Geosciences Paris Sud Department, Paris Sud University, Bâtiment 504, Orsay Cedex, 91405, France IMPMC, Museum National d'histoire Naturelle, Sorbonne Universités, CNRS, UPMC, IRD, 61 Rue Buffon, Paris, 75005, France Cited By :4 Export Date: 9 September 2021 Correspondence Address: Créon, L.; Universidad Nacional Autónoma de México, Campus Juriquilla, A.P. 1-742, Boulevard Juriquila No. 3001, Mexico; email: lauracreon@gmail.com Funding details: Université Pierre et Marie Curie, UPMC Funding text 1: This project was funded by IFP Energies nouvelles. Thank you to Csaba Szab? for his kind help in the field and in the study of these mantle xenoliths. Herman Ravalojaona is acknowledged for his assistance during sample and thin section preparation. We are grateful to Carole La for her efficient help in LA-ICP-MS analyses of trace elements at LPG Nantes. Michel Fialin and Nicolas Rividi of the centre CAMPARIS at UPMC are acknowledged for their assistance for EPMA analyses. We acknowledge Massimo Coltorti and an anonymous reviewer for their comments which greatly improved the manuscript. Paul Asimow provided a final reading and correction of the manuscript. LA - English DB - MTMT ER -