@article{MTMT:34542316, title = {Traces of collisional and transtensional processes between the Carpathia and the European platform in the geoelectric image (NE Slovakia and SE Poland)}, url = {https://m2.mtmt.hu/api/publication/34542316}, author = {Bezak, Vladimir and Ondrasova, Lenka and Vozar, Jan and Orynski, Szymon and Madzin, Jozef and Majcin, Dusan and Klanica, Radek and Bilcik, Dusan}, doi = {10.1007/s11600-023-01239-6}, journal-iso = {ACTA GEOPHYS}, journal = {ACTA GEOPHYSICA}, unique-id = {34542316}, issn = {1895-6572}, abstract = {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.}, keywords = {EVOLUTION; DECOMPOSITION; SUBDUCTION; Western Carpathians; Western Carpathians; BOHEMIAN MASSIF; Pieniny Klippen Belt; Crustal structure; geological structure; Magnetotelluric sounding; Contact zone; Outer Carpathians; Flysch Belt}, year = {2024}, eissn = {1895-7455}, orcid-numbers = {Orynski, Szymon/0000-0001-5764-4876} } @article{MTMT:34399598, title = {Seismic attenuation tomography of Eastern Europe from ambient seismic noise analysis}, url = {https://m2.mtmt.hu/api/publication/34399598}, author = {Borleanu, F and Petrescu, L and Placinta, AO and Magrini, F and Grecu, B and Radulian, M and De Siena, L}, doi = {10.1093/gji/ggad408}, journal-iso = {GEOPHYS J INT}, journal = {GEOPHYSICAL JOURNAL INTERNATIONAL}, volume = {236}, unique-id = {34399598}, issn = {0956-540X}, abstract = {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.}, year = {2024}, eissn = {1365-246X}, pages = {547-564}, orcid-numbers = {Borleanu, F/0000-0001-8502-1422; Petrescu, L/0000-0001-5462-4546; Magrini, F/0000-0003-2417-2686} } @article{MTMT:34412174, title = {Lithostratigraphy of the ignimbrite-dominated Miocene Bükk Foreland Volcanic Area (Central Europe)}, url = {https://m2.mtmt.hu/api/publication/34412174}, author = {Hencz, Mátyás and Biró, Tamás and Németh, Károly and Szakács, Alexandru and Portnyagin, Maxim and Cseri, Zoltán and Pécskay, Zoltán and Szabó, Csaba and Müller, Samuel and Karátson, Dávid}, doi = {10.1016/j.jvolgeores.2023.107960}, journal-iso = {J VOLCANOL GEOTH RES}, journal = {JOURNAL OF VOLCANOLOGY AND GEOTHERMAL RESEARCH}, volume = {445}, unique-id = {34412174}, issn = {0377-0273}, abstract = {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.}, keywords = {STRATIGRAPHY; phreatomagmatism; ignimbrite; Correlation; lithostratigraphy; Glass geochemistry; Volcanic geology; Reworked pyroclasts}, year = {2024}, eissn = {1872-6097}, orcid-numbers = {Hencz, Mátyás/0000-0001-9716-5714; Biró, Tamás/0000-0001-5198-7210; Szabó, Csaba/0000-0002-1580-6344; Karátson, Dávid/0000-0003-0386-1239} } @article{MTMT:33920037, title = {Geological and tectonic interpretation of the new Bouguer gravity anomaly map of Slovakia}, url = {https://m2.mtmt.hu/api/publication/33920037}, author = {Bezak, Vladimir and Bielik, Miroslav and Marko, Frantisek and Zahorec, Pavol and Pasteka, Roman and Vozar, Jan and Papco, Juraj}, doi = {10.31577/GeolCarp.2023.08}, journal-iso = {GEOL CARPATH}, journal = {GEOLOGICA CARPATHICA}, volume = {74}, unique-id = {33920037}, issn = {1335-0552}, abstract = {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.}, keywords = {Slovakia; Tectonics; Western Carpathians; Geology; complete Bouguer gravity anomalies}, year = {2023}, eissn = {1336-8052}, pages = {109-122} } @article{MTMT:33539754, title = {Tracing widespread Early Miocene ignimbrite eruptions and petrogenesis at the onset of the Carpathian-Pannonian Region silicic volcanism}, url = {https://m2.mtmt.hu/api/publication/33539754}, author = {Brlek, M and Tapste, RS and Schindlbeck-Belo, J and Gaynor, SP. and Kutterolf, S and Hauff, F and Georgiev, SV. and Trinajstić, N and Šuica, S and Brčić, V and Wang, KL and Lee, HY and Beier, C and Abersteiner, AB. and Mišur, I and Peytcheva, I and Kukoč, D and Németh, Bianka and Trajanova, M and Balen, D and Guillong, M and Szymanowski, D and Haranginé Lukács, Réka}, doi = {10.1016/j.gr.2022.12.015}, journal-iso = {GONDWANA RES}, journal = {GONDWANA RESEARCH}, volume = {116}, unique-id = {33539754}, issn = {1342-937X}, abstract = {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.}, keywords = {petrogenesis; Tephrostratigraphy; CA-ID-TIMS U-Pb geochronology; Volcanic glass chemistry; Hf and Nd isotope tracers}, year = {2023}, eissn = {1878-0571}, pages = {40-60}, orcid-numbers = {Németh, Bianka/0000-0001-9079-9773; Haranginé Lukács, Réka/0000-0002-2338-4209} } @article{MTMT:34052385, title = {Wide-ranging and violent volcanic history of a quiet transborder area : volcanic geoheritage of the Novohrad–Nógrád UNESCO Global Geopark}, url = {https://m2.mtmt.hu/api/publication/34052385}, author = {Harangi, Szabolcs and Szarvas, I and Haranginé Lukács, Réka}, doi = {10.30486/gcr.2023.1982587.1133}, journal-iso = {GEOCONSERVATION RES}, journal = {GEOCONSERVATION RESEARCH}, volume = {6}, unique-id = {34052385}, issn = {2588-7343}, abstract = {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.}, keywords = {ignimbrite; Columnar jointing; geotourism; Geoeducation; Novohrad-Nógrád UNESCO Global Geopark; monogenetic basalt volcanic field; volcanic root zones}, year = {2023}, eissn = {2645-4661}, pages = {178-206}, orcid-numbers = {Harangi, Szabolcs/0000-0003-2372-4581; Haranginé Lukács, Réka/0000-0002-2338-4209} } @article{MTMT:34210603, title = {Tectonically-determined distribution of monogenetic volcanoes in a compressive tectonic regime: An example from the Pannonian continental back-arc system (Central Europe)}, url = {https://m2.mtmt.hu/api/publication/34210603}, author = {Hencz, Mátyás and Biró, Tamás and Németh, Károly and Porkoláb, Kristóf and Kovács, István János and Spránitz, Tamás and Cloetingh, Sierd and Szabó, Csaba and Berkesi, Márta}, doi = {10.1016/j.jvolgeores.2023.107940}, journal-iso = {J VOLCANOL GEOTH RES}, journal = {JOURNAL OF VOLCANOLOGY AND GEOTHERMAL RESEARCH}, volume = {444}, unique-id = {34210603}, issn = {0377-0273}, abstract = {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.}, keywords = {GIS; FAULT; monogenetic; lithosphere; compression; Bakony-Balaton Highland; lineament}, year = {2023}, eissn = {1872-6097}, pages = {107940-107958}, orcid-numbers = {Hencz, Mátyás/0000-0001-9716-5714; Biró, Tamás/0000-0001-5198-7210; Porkoláb, Kristóf/0000-0001-7470-8296; Spránitz, Tamás/0000-0002-5086-3133; Szabó, Csaba/0000-0002-1580-6344; Berkesi, Márta/0000-0003-4380-057X} } @article{MTMT:33126810, title = {Origin, timing and paleogeographic implications of Paleogene karst bauxites in the northern Transdanubian range, Hungary}, url = {https://m2.mtmt.hu/api/publication/33126810}, author = {Kelemen, Péter and Dunkl, István and Csillag, Gábor and Mindszenty, Andrea and Józsa, Sándor and Fodor, László and von Eynatten, Hilmar}, doi = {10.1007/s00531-022-02249-3}, journal-iso = {INT J EARTH SCI}, journal = {INTERNATIONAL JOURNAL OF EARTH SCIENCES}, volume = {112}, unique-id = {33126810}, issn = {1437-3254}, abstract = {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.}, year = {2023}, eissn = {1437-3262}, pages = {243-264}, orcid-numbers = {Mindszenty, Andrea/0000-0001-8927-3053; Józsa, Sándor/0000-0001-8219-0044} } @article{MTMT:34145447, title = {Thermal Conductivity of Sediments from Well-Logs and its Application to Determine Heat Flow Density in the Pannonian Basin, Hungary}, url = {https://m2.mtmt.hu/api/publication/34145447}, author = {Mihályka, János and Paróczi, Petra and Balázs, László and Drahos, Dezső and Lenkey, László}, doi = {10.1016/j.tecto.2023.230095}, journal-iso = {TECTONOPHYSICS}, journal = {TECTONOPHYSICS}, volume = {868}, unique-id = {34145447}, issn = {0040-1951}, year = {2023}, eissn = {1879-3266}, orcid-numbers = {Paróczi, Petra/0000-0002-5462-7859; Balázs, László/0000-0003-1544-5734; Lenkey, László/0000-0003-4236-4075} } @article{MTMT:33850430, title = {Construction of the Ukrainian Carpathian wedge from low-temperature thermochronology and tectono-stratigraphic analysis}, url = {https://m2.mtmt.hu/api/publication/33850430}, author = {Roger, Marion and de Leeuw, Arjan and van der Beek, Peter and Husson, Laurent and Sobel, Edward R. and Glodny, Johannes and Bernet, Matthias}, doi = {10.5194/se-14-153-2023}, journal-iso = {SOLID EARTH}, journal = {SOLID EARTH}, volume = {14}, unique-id = {33850430}, issn = {1869-9510}, abstract = {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.}, year = {2023}, eissn = {1869-9529}, pages = {153-179} } @article{MTMT:34153996, title = {Provenance and depositional environment of Middle Miocene silicic volcaniclastic deposits from Mt. Medvednica (North Croatian Basin, Carpathian-Pannonian Region)}, url = {https://m2.mtmt.hu/api/publication/34153996}, author = {Trinajstić, N and Brlek, M and Gaynor, SP. and Schindlbeck-Belo, J and Šuica, S and Avanić, R and Kutterolf, S and Wang, KL and Lee, HY and Holcová, K and Kopecká, J and Baranyi, V and Hajek-Tadesse, V and Bakrač, K and Brčić, V and Kukoč, D and Milošević, M and Mišur, I and Haranginé Lukács, Réka}, doi = {10.1016/j.jvolgeores.2023.107917}, journal-iso = {J VOLCANOL GEOTH RES}, journal = {JOURNAL OF VOLCANOLOGY AND GEOTHERMAL RESEARCH}, volume = {443}, unique-id = {34153996}, issn = {0377-0273}, year = {2023}, eissn = {1872-6097}, orcid-numbers = {Haranginé Lukács, Réka/0000-0002-2338-4209} } @article{MTMT:33189026, title = {From dysoxic sea to hypersaline lagoon: Paleoenvironmental changes on the Badenian/Sarmatian boundary (borehole MZ102; Vienna basin)}, url = {https://m2.mtmt.hu/api/publication/33189026}, author = {Babejová-Kmecová, J. and Plašienková, I. and Sliva, L. and Halásová, E. and Hudácková, N.}, journal-iso = {ACTA GEOL SLOV}, journal = {ACTA GEOLOGICA SLOVACA}, volume = {14}, unique-id = {33189026}, issn = {1338-0044}, year = {2022}, eissn = {1338-5674}, pages = {57-72} } @article{MTMT:33541001, title = {A review of geophysical studies of the lithosphere in the Carpathian–Pannonian region}, url = {https://m2.mtmt.hu/api/publication/33541001}, author = {Bielik, Miroslav and Zeyen, Herman and Starostenko, Vitaly and Makarenko, Irina and Legostaeva, Olga and Savchenko, Sasha and Dérerová, Jana and Grinč, Michal and Godová, Dominika and Pánisová, Jaroslava}, doi = {10.31577/GeolCarp.73.6.2}, journal-iso = {GEOL CARPATH}, journal = {GEOLOGICA CARPATHICA}, volume = {73}, unique-id = {33541001}, issn = {1335-0552}, year = {2022}, eissn = {1336-8052}, pages = {499-516}, orcid-numbers = {Bielik, Miroslav/0000-0003-2792-7669; Zeyen, Herman/0000-0003-1820-9032; Starostenko, Vitaly/0000-0002-7960-0011; Makarenko, Irina/0000-0002-8919-2218; Dérerová, Jana/0000-0002-4855-6433; Godová, Dominika/0000-0002-7811-2825; Pánisová, Jaroslava/0000-0002-6608-0918} } @article{MTMT:33535625, title = {Geochronology, geochemistry, and geodynamic evolution of Tatric granites from crystallization to exhumation (Tatra Mountains, Western Carpathians)}, url = {https://m2.mtmt.hu/api/publication/33535625}, author = {Catlos, EJ. and Broska, I and Kohút, M and Etzel, TM. and Kyle, JR and Stockli, DF. and Miggins, DP and Campos, D}, doi = {10.31577/GeolCarp.73.6.1}, journal-iso = {GEOL CARPATH}, journal = {GEOLOGICA CARPATHICA}, volume = {73}, unique-id = {33535625}, issn = {1335-0552}, year = {2022}, eissn = {1336-8052}, pages = {517-544}, orcid-numbers = {Catlos, EJ./0000-0001-6043-3498; Broska, I/0000-0002-8464-8976; Kohút, M/0000-0001-5749-4732; Etzel, TM./0000-0002-8593-718X; Kyle, JR/0000-0002-5319-8941; Stockli, DF./0000-0001-7652-2129; Miggins, DP/0000-0001-8256-8377} } @article{MTMT:32930743, title = {Wide Versus Narrow Back-Arc Rifting: Control of Subduction Velocity and Convective Back-Arc Thinning}, url = {https://m2.mtmt.hu/api/publication/32930743}, author = {Erdős, Zoltán and Huismans, RS and Faccenna, C}, doi = {10.1029/2021TC007086}, journal-iso = {TECTONICS}, journal = {TECTONICS}, volume = {41}, unique-id = {32930743}, issn = {0278-7407}, year = {2022}, eissn = {1944-9194}, orcid-numbers = {Erdős, Zoltán/0000-0002-7974-7179} } @article{MTMT:33037042, title = {Historical fog climate dataset for Carpathian Basin from 1886 to 1919}, url = {https://m2.mtmt.hu/api/publication/33037042}, author = {Gandhi, Arun and Bartók, Blanka and Musyimi, Peter Kinyae and Ilona, Judit and Weidinger, Tamás}, doi = {10.1016/j.dib.2022.108500}, journal-iso = {DATA BRIEF}, journal = {DATA IN BRIEF}, volume = {44}, unique-id = {33037042}, year = {2022}, eissn = {2352-3409}, orcid-numbers = {Weidinger, Tamás/0000-0001-7500-6579} } @article{MTMT:33167952, title = {Melange, Flysch and Cliffs in the Pieniny Klippen Belt (Poland): An Overview}, url = {https://m2.mtmt.hu/api/publication/33167952}, author = {Golonka, Jan and Waskowska, Anna and Cichostepski, Kamil and Dec, Jerzy and Pietsch, Kaja and Loj, Monika and Bania, Grzegorz and Moscicki, Wlodzimierz Jerzy and Porzucek, Slawomir}, doi = {10.3390/min12091149}, journal-iso = {MINERALS-BASEL}, journal = {MINERALS}, volume = {12}, unique-id = {33167952}, abstract = {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.}, keywords = {melange; Tectonics; Pieniny Klippen Belt; flysch; Magura Nappe; Central Carpathians; North European platform}, year = {2022}, eissn = {2075-163X}, orcid-numbers = {Waskowska, Anna/0000-0003-4090-8534; Cichostepski, Kamil/0000-0001-7982-4763; Dec, Jerzy/0000-0002-2911-5771; Bania, Grzegorz/0000-0002-9661-8184; Porzucek, Slawomir/0000-0002-8250-2703} } @article{MTMT:32529867, title = {Strain partitioning in a large intracontinental strike-slip system accommodating backarc-convex orocline formation: The Circum-Moesian Fault System of the Carpatho-Balkanides}, url = {https://m2.mtmt.hu/api/publication/32529867}, author = {Krstekanić, Nemanja and Matenco, Liviu and Stojadinovic, Uros and Willingshofer, Ernst and Toljić, Marinko and Tamminga, Daan}, doi = {10.1016/j.gloplacha.2021.103714}, journal-iso = {GLOBAL PLANET CHANGE}, journal = {GLOBAL AND PLANETARY CHANGE}, volume = {208}, unique-id = {32529867}, issn = {0921-8181}, year = {2022}, eissn = {1872-6364} } @article{MTMT:32787471, title = {Formal definition and description of lithostratigraphic units related to the Miocene silicic pyroclastic rocks outcropping in Northern Hungary: a revision}, url = {https://m2.mtmt.hu/api/publication/32787471}, author = {Haranginé Lukács, Réka and Harangi, Szabolcs and Gál, Péter and Szepesi, János and Di Capua, A and Norini, G and Sulpizio, R and Groppelli, G and Fodor, László}, doi = {10.31577/GeolCarp.73.2.3}, journal-iso = {GEOL CARPATH}, journal = {GEOLOGICA CARPATHICA}, volume = {73}, unique-id = {32787471}, issn = {1335-0552}, year = {2022}, eissn = {1336-8052}, pages = {137-158}, orcid-numbers = {Haranginé Lukács, Réka/0000-0002-2338-4209; Harangi, Szabolcs/0000-0003-2372-4581} } @article{MTMT:34518697, title = {Dachiardite-Ca, ferrierite-Mg and associated zeolite mineralization in chalcedony cavities from localities Byšta, Brezina and Kuzmice (Slanské vrchy Mts., Slovak Republic)}, url = {https://m2.mtmt.hu/api/publication/34518697}, author = {Myšľan, P. and Števko, M. and Sejkora, J. and Dolníček, Z.}, doi = {10.46861/bmp.30.045}, journal-iso = {Bull Mineral Petrolog}, journal = {Bulletin Mineralogie Petrologie}, volume = {30}, unique-id = {34518697}, issn = {2570-7337}, year = {2022}, eissn = {2570-7345}, pages = {45-60} } @article{MTMT:32915030, title = {Rotation at subduction margins: How complexity at fault-scale (the 2019 Albanian Mw 6.4 earthquake) mirrors the regional deformation}, url = {https://m2.mtmt.hu/api/publication/32915030}, author = {Pezzo, G. and Palano, M. and Chiarabba, C.}, doi = {10.1111/ter.12584}, journal-iso = {TERRA NOVA}, journal = {TERRA NOVA}, volume = {34}, unique-id = {32915030}, issn = {0954-4879}, year = {2022}, eissn = {1365-3121}, pages = {244-252} } @article{MTMT:33025440, title = {Volcanic Landforms and Landscapes of the East Carpathians (Romania) and Their Geoheritage Values}, url = {https://m2.mtmt.hu/api/publication/33025440}, author = {Szakács, A and Kovacs, M}, doi = {10.3390/land11071064}, journal-iso = {LAND-BASEL}, journal = {LAND (BASEL)}, volume = {11}, unique-id = {33025440}, year = {2022}, eissn = {2073-445X} } @article{MTMT:32893701, title = {Deltaic systems of the northern Vienna Basin: The lower-middle Miocene conglomerate bodies}, url = {https://m2.mtmt.hu/api/publication/32893701}, author = {Tamás, Csibri and Andrej, Ruman and Natalia, Hudackova and Michal, Jamrich and L'ubomir, Sliva and Katarína, Šarinová and Michal, Kovac}, doi = {10.31577/GeolCarp.73.3.5}, journal-iso = {GEOL CARPATH}, journal = {GEOLOGICA CARPATHICA}, volume = {73}, unique-id = {32893701}, issn = {1335-0552}, year = {2022}, eissn = {1336-8052}, pages = {245-269} } @{MTMT:32825822, title = {Outline of Geology and Cenozoic Evolution of Slovakia}, url = {https://m2.mtmt.hu/api/publication/32825822}, author = {Vojtko, R and Plašienka, D and Kováč, M}, booktitle = {Landscapes and Landforms of Slovakia}, doi = {10.1007/978-3-030-89293-7_2}, unique-id = {32825822}, year = {2022}, pages = {9-26} } @article{MTMT:32272626, title = {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}, url = {https://m2.mtmt.hu/api/publication/32272626}, author = {Bezak, Vladimir and Vozar, Jan and Majcin, Dusan and Klanica, Radek and Madaras, Jan}, doi = {10.7306/gq.1595}, journal-iso = {GEOL Q}, journal = {GEOLOGICAL QUARTERLY}, volume = {65}, unique-id = {32272626}, issn = {1641-7291}, abstract = {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.}, keywords = {SUBDUCTION; Western Carpathians; collision; Magnetotelluric sounding; Transpression; Klippen Belt; deep structures}, year = {2021}, eissn = {2082-5099} } @article{MTMT:32279975, title = {Petrological characteristics of clastic sedimentary rocks from the St. Barbara ore mine in Rude near Samobor}, url = {https://m2.mtmt.hu/api/publication/32279975}, author = {Bilic, Sime and Garasic, Vesnica}, doi = {10.17794/rgn.2021.1.10}, journal-iso = {RUDARSKO GEOLOSKO NAFTNI ZBORNIK - MIN GEOL PETROL ENG BULL}, journal = {RUDARSKO GEOLOSKO NAFTNI ZBORNIK - MINING GELOLOGICAL PETROLEUM ENGINEERING BULLETIN}, volume = {36}, unique-id = {32279975}, issn = {0353-4529}, abstract = {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.}, keywords = {PROVENANCE; clastic sedimentary rocks; petrography and geochemistry; St. Barbara ore mine in Rude; Samobor Mountains}, year = {2021}, eissn = {1849-0409}, pages = {121-135} } @article{MTMT:32348229, title = {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)}, url = {https://m2.mtmt.hu/api/publication/32348229}, author = {Botor, Dariusz}, doi = {10.3390/min11070733}, journal-iso = {MINERALS-BASEL}, journal = {MINERALS}, volume = {11}, unique-id = {32348229}, abstract = {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.}, keywords = {carpathians; hydrocarbon generation; maturity modeling; Carpathians Foredeep; Paleozoic-Mesozoic basement; petroleum origin}, year = {2021}, eissn = {2075-163X}, orcid-numbers = {Botor, Dariusz/0000-0003-0157-4885} } @article{MTMT:32915031, title = {Rheological model of the lithosphere along profile VII in the Eastern Carpathians}, url = {https://m2.mtmt.hu/api/publication/32915031}, author = {DEREROVA, J. and BIELIK, M. and KOHUT, I. and GODOVA, D. and MOJZES, A.}, doi = {10.31577/congeo.2021.51.3.3}, journal-iso = {CONTRIB GEOPHYS GEODES}, journal = {CONTRIBUTIONS TO GEOPHYSICS AND GEODESY}, volume = {51}, unique-id = {32915031}, issn = {1335-2806}, year = {2021}, pages = {245-263} } @article{MTMT:31846118, title = {Correlating volcanic dynamics and the construction of a submarine volcanogenic apron: An example from the Badenian (Middle Miocene) of North-Eastern Hungary}, url = {https://m2.mtmt.hu/api/publication/31846118}, author = {Di Capua, A. and Barilaro, F. and Szepesi, János and Haranginé Lukács, Réka and Gál, Péter and Norini, G. and Sulpizio, R. and Soós, Ildikó and Harangi, Szabolcs and Groppelli, G.}, doi = {10.1016/j.marpetgeo.2021.104944}, journal-iso = {MAR PETROL GEOL}, journal = {MARINE AND PETROLEUM GEOLOGY}, volume = {126}, unique-id = {31846118}, issn = {0264-8172}, year = {2021}, eissn = {1873-4073}, orcid-numbers = {Haranginé Lukács, Réka/0000-0002-2338-4209; Gál, Péter/0000-0002-2811-8460; Soós, Ildikó/0000-0003-2345-8391; Harangi, Szabolcs/0000-0003-2372-4581} } @article{MTMT:32112689, title = {The role of subduction interface and upper plate strength on back‐arc extension: application to Mediterranean back‐arc basins}, url = {https://m2.mtmt.hu/api/publication/32112689}, author = {Erdős, Zoltán and Huismans, Ritske S. and Faccenna, Claudio and Wolf, Sebastian G.}, doi = {10.1029/2021TC006795}, journal-iso = {TECTONICS}, journal = {TECTONICS}, volume = {40}, unique-id = {32112689}, issn = {0278-7407}, year = {2021}, eissn = {1944-9194}, orcid-numbers = {Erdős, Zoltán/0000-0002-7974-7179; Huismans, Ritske S./0000-0003-0548-6591; Faccenna, Claudio/0000-0003-0765-4165; Wolf, Sebastian G./0000-0001-8897-9214} } @article{MTMT:31936855, title = {Crustal exhumation and depocenter migration from the Alpine orogenic margin towards the Pannonian extensional back-arc basin controlled by inheritance}, url = {https://m2.mtmt.hu/api/publication/31936855}, author = {Fodor, László and Balázs, Attila and Csillag, Gábor and Dunkl, István and Héja, Gábor and Jelen, B and Kelemen, Péter and Kövér, Szilvia and Németh, A and Nyíri, D and Selmeczi, Ildikó and Trajanova, M and Vrabec, M and Vrabec, M}, doi = {10.1016/j.gloplacha.2021.103475}, journal-iso = {GLOBAL PLANET CHANGE}, journal = {GLOBAL AND PLANETARY CHANGE}, volume = {201}, unique-id = {31936855}, issn = {0921-8181}, year = {2021}, eissn = {1872-6364}, orcid-numbers = {Balázs, Attila/0000-0003-2948-0397; Kövér, Szilvia/0000-0002-6736-4226} } @article{MTMT:31929072, title = {A Lower Miocene pyroclastic-fall deposit from the Bukk Foreland Volcanic Area, Northern Hungary: Clues for an eastward-located source}, url = {https://m2.mtmt.hu/api/publication/31929072}, author = {Hencz, Mátyás and Biró, Tamás and Cseri, Zoltán and Karátson, Dávid and Márton Péterné Szalay, Emőke and Németh, Károly and Szakács, Alexandru and Pécskay, Zoltán and Kovács, István János}, doi = {10.31577/GeolCarp.72.1.3}, journal-iso = {GEOL CARPATH}, journal = {GEOLOGICA CARPATHICA}, volume = {72}, unique-id = {31929072}, issn = {1335-0552}, abstract = {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.}, keywords = {Paleomagnetism; granulometry; Plinian; Ignimbrites; Source region; volcano stratigraphy; pyroclastic fall}, year = {2021}, eissn = {1336-8052}, pages = {26-47}, orcid-numbers = {Hencz, Mátyás/0000-0001-9716-5714; Biró, Tamás/0000-0001-5198-7210; Karátson, Dávid/0000-0003-0386-1239; Márton Péterné Szalay, Emőke/0000-0002-2135-8867; Kovács, István János/0000-0002-3488-3716} } @article{MTMT:32239855, title = {Uniform “water” content in quartz phenocrysts from silicic pyroclastic fallout deposits – implications on pre-eruptive conditions}, url = {https://m2.mtmt.hu/api/publication/32239855}, author = {Hencz, Mátyás and Biró, Tamás and Kovács, István János and Stalder, R. and Németh, Károly and Szakács, Alexandru and Pálos, Zsófia and Pécskay, Zoltán and Karátson, Dávid}, doi = {10.5194/ejm-33-571-2021}, journal-iso = {EUR J MINERAL}, journal = {EUROPEAN JOURNAL OF MINERALOGY}, volume = {33}, unique-id = {32239855}, issn = {0935-1221}, year = {2021}, eissn = {1617-4011}, pages = {571-589}, orcid-numbers = {Hencz, Mátyás/0000-0001-9716-5714; Biró, Tamás/0000-0001-5198-7210; Kovács, István János/0000-0002-3488-3716; Karátson, Dávid/0000-0003-0386-1239} } @article{MTMT:31655214, title = {Structural contraints of neotectonic activity in the eastern part of the western carpathians orogenic wedge}, url = {https://m2.mtmt.hu/api/publication/31655214}, author = {Jacko, S. and Jacko sen, S. and Labant, S. and Bátorová, K. and Farkašovský, R. and Ščerbáková, B.}, doi = {10.1016/j.quaint.2020.10.072}, journal-iso = {QUATERN INT}, journal = {QUATERNARY INTERNATIONAL}, volume = {585}, unique-id = {31655214}, issn = {1040-6182}, year = {2021}, eissn = {1873-4553}, pages = {27-43} } @article{MTMT:32055044, title = {Contrasting metamorphic and post-metamorphic evolutions within the Algyő basement high (Tisza Mega-unit, SE Hungary). Consequences for structural history}, url = {https://m2.mtmt.hu/api/publication/32055044}, author = {Kondor, Henrietta and M. Tóth, Tivadar}, doi = {10.1556/24.2021.00004}, journal-iso = {CENT EUR GEOL}, journal = {CENTRAL EUROPEAN GEOLOGY}, volume = {64}, unique-id = {32055044}, issn = {1788-2281}, year = {2021}, eissn = {1789-3348}, pages = {91-112}, orcid-numbers = {Kondor, Henrietta/0000-0001-5103-1083; M. Tóth, Tivadar/0000-0003-1012-1095} } @article{MTMT:32016325, title = {Architecture of volcanic plumbing systems inferred from thermobarometry: A case study from the Miocene Gutâi Volcanic Zone in the Eastern Carpathians, Romania}, url = {https://m2.mtmt.hu/api/publication/32016325}, author = {Kovacs, M and Fülöp, A and Seghedi, I and Pécskay, Zoltán}, doi = {10.1016/j.lithos.2021.106191}, journal-iso = {LITHOS}, journal = {LITHOS}, volume = {396-397}, unique-id = {32016325}, issn = {0024-4937}, year = {2021}, eissn = {1872-6143} } @article{MTMT:31711317, title = {Occurrence and significance of smectite in the Pliensbachian (Lower Jurassic) at Lókút 2 (Bakony Mts., Hungary)}, url = {https://m2.mtmt.hu/api/publication/31711317}, author = {Leskó, Máté Zsigmond and Papp, Richárd Zoltán and Kristály, Ferenc and Pálfy, József and Zajzon, Norbert}, doi = {10.1556/24.2021.00002}, journal-iso = {CENT EUR GEOL}, journal = {CENTRAL EUROPEAN GEOLOGY}, volume = {64}, unique-id = {31711317}, issn = {1788-2281}, year = {2021}, eissn = {1789-3348}, pages = {8-17}, orcid-numbers = {Kristály, Ferenc/0000-0002-0075-5994; Pálfy, József/0000-0001-9686-1849} } @article{MTMT:31956559, title = {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}, url = {https://m2.mtmt.hu/api/publication/31956559}, author = {Liptai, Nóra and Berkesi, Márta and Patkó, Levente and Bodnár, RJ and O’Reilly, SY and Griffin, WL and Szabó, Csaba}, doi = {10.2138/am-2021-7292}, journal-iso = {AM MINERAL}, journal = {AMERICAN MINERALOGIST}, volume = {106}, unique-id = {31956559}, issn = {0003-004X}, year = {2021}, eissn = {1945-3027}, pages = {685-700}, orcid-numbers = {Liptai, Nóra/0000-0002-2464-2468; Berkesi, Márta/0000-0003-4380-057X; Patkó, Levente/0000-0001-6007-3103; Szabó, Csaba/0000-0002-1580-6344} } @article{MTMT:31655281, title = {Effect of water on the rheology of the lithospheric mantle in young extensional basin systems as shown by xenoliths from the Carpathian-Pannonian region}, url = {https://m2.mtmt.hu/api/publication/31655281}, author = {Liptai, Nóra and Lange, Thomas Pieter and Patkó, Levente and Pintér, Zsanett and Berkesi, Márta and Aradi, László Előd and Szabó, Csaba and Kovács, István János}, doi = {10.1016/j.gloplacha.2020.103364}, journal-iso = {GLOBAL PLANET CHANGE}, journal = {GLOBAL AND PLANETARY CHANGE}, volume = {196}, unique-id = {31655281}, issn = {0921-8181}, year = {2021}, eissn = {1872-6364}, orcid-numbers = {Liptai, Nóra/0000-0002-2464-2468; Lange, Thomas Pieter/0000-0002-8709-9239; Patkó, Levente/0000-0001-6007-3103; Berkesi, Márta/0000-0003-4380-057X; Aradi, László Előd/0000-0003-0276-3119; Szabó, Csaba/0000-0002-1580-6344; Kovács, István János/0000-0002-3488-3716} } @article{MTMT:32078777, title = {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}, url = {https://m2.mtmt.hu/api/publication/32078777}, author = {Hargitainé Molnár, Zsuzsa and Baloghné Kiss, Gabriella and Molnár, Ferenc and Váczi, Tamás and Czuppon, György and Dunkl, István and Zaccarini, F. and Dódony, István}, doi = {10.3390/min11060640}, journal-iso = {MINERALS-BASEL}, journal = {MINERALS}, volume = {11}, unique-id = {32078777}, year = {2021}, eissn = {2075-163X}, orcid-numbers = {Baloghné Kiss, Gabriella/0000-0002-7162-2961; Molnár, Ferenc/0000-0002-1873-1915; Váczi, Tamás/0000-0003-0142-545X; Czuppon, György/0000-0002-7231-6042} } @article{MTMT:31930222, title = {Magnitude Estimation of Overpressure Generation Mechanisms Using Quantitative Stochastic 2D Basin Models: A Case Study from the Danube-Tisza Interfluve Area in Hungary}, url = {https://m2.mtmt.hu/api/publication/31930222}, author = {Nagy, Zsolt and Baracza, Mátyás Krisztián and Szabó, Norbert Péter}, doi = {10.3390/app11062841}, journal-iso = {APPL SCI-BASEL}, journal = {APPLIED SCIENCES-BASEL}, volume = {11}, unique-id = {31930222}, year = {2021}, eissn = {2076-3417} } @article{MTMT:32116865, title = {Melt-rock interaction in the lower crust based on silicate melt inclusions in mafic garnet granulite xenoliths, Bakony-Balaton Highland Volcanic Field (Hungary)}, url = {https://m2.mtmt.hu/api/publication/32116865}, author = {Németh, Bianka and Török, Kálmán and Bali, E and Zajacz, Z and Fodor, László and Szabó, Csaba}, doi = {10.31577/GeolCarp.72.3.4}, journal-iso = {GEOL CARPATH}, journal = {GEOLOGICA CARPATHICA}, volume = {72}, unique-id = {32116865}, issn = {1335-0552}, abstract = {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.}, keywords = {Trace Elements; Silicate melt inclusion; crustal contamination; partial melting; Anatexis; Mafic granulite; peraluminous granitoid melt}, year = {2021}, eissn = {1336-8052}, pages = {232-252}, orcid-numbers = {Németh, Bianka/0000-0001-9079-9773; Szabó, Csaba/0000-0002-1580-6344} } @article{MTMT:32075619, title = {Paleogeographic implications of a multi-parameter Paleogene provenance dataset (Transylvanian Basin, Romania)}, url = {https://m2.mtmt.hu/api/publication/32075619}, author = {Obbágy, Gabriella and Dunkl, István and Józsa, Sándor and Silye, Lóránd and Arató, Róbert and Lünsdorf, NK and von Eynatten, H}, doi = {10.2110/jsr.2020.080}, journal-iso = {J SEDIMENT RES}, journal = {JOURNAL OF SEDIMENTARY RESEARCH}, volume = {91}, unique-id = {32075619}, issn = {1527-1404}, year = {2021}, eissn = {1938-3681}, pages = {551-570}, orcid-numbers = {Józsa, Sándor/0000-0001-8219-0044; Silye, Lóránd/0000-0001-7306-6041} } @article{MTMT:31659943, title = {The polyphase rifting and inversion of the Danube Basin revised}, url = {https://m2.mtmt.hu/api/publication/31659943}, author = {Šujan, M and Rybár, S and Kováč, M and Bielik, M and Majcin, D and Minár, J and Plašienka, D and Nováková, P and Kotulová, J}, doi = {10.1016/j.gloplacha.2020.103375}, journal-iso = {GLOBAL PLANET CHANGE}, journal = {GLOBAL AND PLANETARY CHANGE}, volume = {196}, unique-id = {31659943}, issn = {0921-8181}, year = {2021}, eissn = {1872-6364} } @article{MTMT:32558406, title = {Petrology and zircon U–Pb dating of granitoid rocks in the Highiş massif (SW Apuseni Mts., Romania): Insights into Permian plutonic–volcanic connections}, url = {https://m2.mtmt.hu/api/publication/32558406}, author = {Szemerédi, Máté and Raucsikné Varga, Andrea Beáta and Dunkl, I. and Haranginé Lukács, Réka and Seghedi, I. and Kovács, Zoltán and Raucsik, Béla and Pál-Molnár, Elemér}, doi = {10.31577/GeolCarp.72.6.3}, journal-iso = {GEOL CARPATH}, journal = {GEOLOGICA CARPATHICA}, volume = {72}, unique-id = {32558406}, issn = {1335-0552}, year = {2021}, eissn = {1336-8052}, pages = {482-504}, orcid-numbers = {Szemerédi, Máté/0000-0002-7432-8418; Raucsikné Varga, Andrea Beáta/0000-0002-8673-1482; Haranginé Lukács, Réka/0000-0002-2338-4209; Raucsik, Béla/0000-0002-1951-5974; Pál-Molnár, Elemér/0000-0002-9606-0133} } @article{MTMT:32236369, title = {Morphotectonic configuration of the Podtatranská Kotlina Basin and its relationship to the origin of the Western Carpathians}, url = {https://m2.mtmt.hu/api/publication/32236369}, author = {Vitovič, L and Minár, J and Pánek, T}, doi = {10.1016/j.geomorph.2021.107963}, journal-iso = {GEOMORPHOLOGY}, journal = {GEOMORPHOLOGY}, volume = {394}, unique-id = {32236369}, issn = {0169-555X}, year = {2021}, eissn = {1872-695X} } @article{MTMT:32318191, title = {Three-dimensional magnetotelluric model along seismic profile 2T: An improved view on crustal structure in central Slovakia (Western Carpathians)}, url = {https://m2.mtmt.hu/api/publication/32318191}, author = {Vozari, Jan and Bezak, Vladimir and Marko, Frantisek}, doi = {10.31577/GeolCarp.72.2.1}, journal-iso = {GEOL CARPATH}, journal = {GEOLOGICA CARPATHICA}, volume = {72}, unique-id = {32318191}, issn = {1335-0552}, abstract = {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.}, keywords = {Western Carpathians; accretionary prism; 3-D magnetotellurics; integrated interpretation; back-thrusting; block boundary faults}, year = {2021}, eissn = {1336-8052}, pages = {85-95} } @article{MTMT:32602387, title = {Thermal Maturity of the Grajcarek Unit (Pieniny Klippen Belt): Insights for the Burial History of a Major Tectonic Boundary of the Western Carpathians}, url = {https://m2.mtmt.hu/api/publication/32602387}, author = {Zielinska, Magdalena}, doi = {10.3390/min11111245}, journal-iso = {MINERALS-BASEL}, journal = {MINERALS}, volume = {11}, unique-id = {32602387}, abstract = {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.}, keywords = {Western Carpathians; Pieniny Klippen Belt; organic matter; Thermal maturity; Vitrinite reflectance; burial depth}, year = {2021}, eissn = {2075-163X}, orcid-numbers = {Zielinska, Magdalena/0000-0003-4210-6543} } @article{MTMT:31437022, title = {Geoelectrically distinct zones in the crust of the Western Carpathians: A consequence of Neogene strike-slip tectonics}, url = {https://m2.mtmt.hu/api/publication/31437022}, author = {Bezak, Vladimir and Pek, Josef and Vozar, Jan and Majcin, Dusan and Bielik, Miroslav and Tomek, Cestmir}, doi = {10.31577/GeolCarp.71.1.2}, journal-iso = {GEOL CARPATH}, journal = {GEOLOGICA CARPATHICA}, volume = {71}, unique-id = {31437022}, issn = {1335-0552}, abstract = {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.}, keywords = {Western Carpathians; magnetotellurics; physically distinct zones; strike-slip tectonics}, year = {2020}, eissn = {1336-8052}, pages = {14-+}, orcid-numbers = {Vozar, Jan/0000-0003-2448-345X} } @article{MTMT:31355974, title = {A Miocene Phreatoplinian eruption in the North-Eastern Pannonian Basin, Hungary : the Jató Member}, url = {https://m2.mtmt.hu/api/publication/31355974}, author = {Biró, Tamás and Hencz, Mátyás and Németh, Károly and Karátson, Dávid and Márton Péterné Szalay, Emőke and Szakács, A and Bradák, Balázs and Szalai, Zoltán and Pécskay, Zoltán and Kovács, István János}, doi = {10.1016/j.jvolgeores.2020.106973}, journal-iso = {J VOLCANOL GEOTH RES}, journal = {JOURNAL OF VOLCANOLOGY AND GEOTHERMAL RESEARCH}, volume = {401}, unique-id = {31355974}, issn = {0377-0273}, year = {2020}, eissn = {1872-6097}, orcid-numbers = {Biró, Tamás/0000-0001-5198-7210; Hencz, Mátyás/0000-0001-9716-5714; Karátson, Dávid/0000-0003-0386-1239; Márton Péterné Szalay, Emőke/0000-0002-2135-8867; Szalai, Zoltán/0000-0001-5267-411X; Kovács, István János/0000-0002-3488-3716} } @article{MTMT:32915033, title = {Lithospheric model along transect HT-1 across Western Carpathians and Pannonian Basin based on 2D integrated modelling}, url = {https://m2.mtmt.hu/api/publication/32915033}, author = {DÉREROVÁ, J. and BIELIK, M. and KOHÚT, I. and GODOVÁ, D. and VOZÁR, J. and BEZÁK, V.}, doi = {10.31577/congeo.2020.50.4.5}, journal-iso = {J TAX}, journal = {JOURNAL OF TAXATION: A NATIONAL JOURNAL OF CURRENT DEVELOPMENTS, ANALYSIS, AND COMMENTARY FOR TAX PROFESSIONALS}, volume = {50}, unique-id = {32915033}, issn = {0022-4863}, year = {2020}, pages = {463-474} } @article{MTMT:31389781, title = {Growth and erosion rates of the East Carpathians volcanoes constrained by numerical models: Tectonic and climatic implications}, url = {https://m2.mtmt.hu/api/publication/31389781}, author = {Dibacto, S. and Lahitte, P. and Karátson, Dávid and Hencz, Mátyás and Szakács, A. and Biró, Tamás and Kovács, István János and Veres, D.}, doi = {10.1016/j.geomorph.2020.107352}, journal-iso = {GEOMORPHOLOGY}, journal = {GEOMORPHOLOGY}, volume = {368}, unique-id = {31389781}, issn = {0169-555X}, year = {2020}, eissn = {1872-695X}, orcid-numbers = {Dibacto, S./0000-0003-0048-3017; Karátson, Dávid/0000-0003-0386-1239; Hencz, Mátyás/0000-0001-9716-5714; Biró, Tamás/0000-0001-5198-7210; Kovács, István János/0000-0002-3488-3716} } @article{MTMT:30899104, title = {Dolomitization of shallow-water, mixed silicilastic‑carbonate sequences: The Lower Triassic ramp succession of the Transdanubian Range, Hungary}, url = {https://m2.mtmt.hu/api/publication/30899104}, author = {Győri, Orsolya and Haas, János and Hips, Kinga and Lukoczki, Georgina and Budai, Tamás and Demény, Attila and Laczkó-Dobos, Emese}, doi = {10.1016/j.sedgeo.2019.105549}, journal-iso = {SEDIMENT GEOL}, journal = {SEDIMENTARY GEOLOGY}, volume = {395}, unique-id = {30899104}, issn = {0037-0738}, abstract = {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.}, year = {2020}, eissn = {1879-0968}, orcid-numbers = {Győri, Orsolya/0000-0002-3646-9113; Haas, János/0000-0003-0929-8889; Hips, Kinga/0000-0003-2315-120X; Lukoczki, Georgina/0000-0002-0661-0198; Demény, Attila/0000-0003-0522-9018} } @article{MTMT:31857278, title = {The Pannonian Basin System northern margin paleogeography, climate and depositional environments in the time range during MMCT (Central Paratethys, Novohrad-Nógrád Basin, Slovakia)}, url = {https://m2.mtmt.hu/api/publication/31857278}, author = {Hudáčková, N and Holcová, K and Halásová, E and Kováčová, M and Doláková, N and Trubač, J and Rybár, S and Ruman, A and Stárek, D and Šujan, M and Jamrich, M and Kováč, M}, doi = {10.26879/1067}, journal-iso = {PALAEONTOL ELECTRON}, journal = {PALAEONTOLOGIA ELECTRONICA}, volume = {23}, unique-id = {31857278}, issn = {1935-3952}, year = {2020}, eissn = {1094-8074} } @article{MTMT:31640869, title = {Geological deformations in the Pannonian Basin during the neotectonic phase: New insights from the latest regional mapping in Hungary}, url = {https://m2.mtmt.hu/api/publication/31640869}, author = {Koroknai, B and Wórum, G and Tóth, T and Koroknai, Zs and Fekete-Németh, V and Kovács, Gábor}, doi = {10.1016/j.earscirev.2020.103411}, journal-iso = {EARTH-SCI REV}, journal = {EARTH-SCIENCE REVIEWS}, volume = {211}, unique-id = {31640869}, issn = {0012-8252}, year = {2020}, eissn = {1872-6828}, orcid-numbers = {Kovács, Gábor/0000-0001-6720-3126} } @article{MTMT:31006469, title = {The role of water and compression in the genesis of alkaline basalts: Inferences from the Carpathian-Pannonian region}, url = {https://m2.mtmt.hu/api/publication/31006469}, author = {Kovács, István János and Patkó, Levente and Liptai, Nóra and Lange, Thomas Pieter and Taracsák, Z. and Cloetingh, S.A.P.L. and Török, Kálmán and Király, Edit and Karátson, Dávid and Biró, Tamás and Kiss, János and Pálos, Zsófia and Aradi, László Előd and Falus, György and Hidas, K. and Berkesi, Márta and Koptev, A. and Novák, Attila and Wesztergom, Viktor and Fancsik, Tamás and Szabó, Csaba}, doi = {10.1016/j.lithos.2019.105323}, journal-iso = {LITHOS}, journal = {LITHOS}, volume = {354-355}, unique-id = {31006469}, issn = {0024-4937}, year = {2020}, eissn = {1872-6143}, orcid-numbers = {Kovács, István János/0000-0002-3488-3716; Patkó, Levente/0000-0001-6007-3103; Liptai, Nóra/0000-0002-2464-2468; Lange, Thomas Pieter/0000-0002-8709-9239; Karátson, Dávid/0000-0003-0386-1239; Biró, Tamás/0000-0001-5198-7210; Kiss, János/0000-0001-8589-1364; Aradi, László Előd/0000-0003-0276-3119; Berkesi, Márta/0000-0003-4380-057X; Szabó, Csaba/0000-0002-1580-6344} } @article{MTMT:31415636, title = {Cu-3(As,Sb)S-4 minerals from the Baia Mare metallogenic district, Eastern Carpathians, Romania - a case study from the Cisma ore deposit}, url = {https://m2.mtmt.hu/api/publication/31415636}, author = {Kovacs, Reka and Tamas, Calin Gabriel}, doi = {10.7306/gq.1529}, journal-iso = {GEOL Q}, journal = {GEOLOGICAL QUARTERLY}, volume = {64}, unique-id = {31415636}, issn = {1641-7291}, abstract = {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.}, keywords = {Enargite; Herja; luzonite; Cisma; Baiut; Baia Mare metallogenic district}, year = {2020}, eissn = {2082-5099}, pages = {263-274} } @article{MTMT:31651888, title = {Understanding partitioning of deformation in highly arcuate orogenic systems: Inferences from the evolution of the Serbian Carpathians}, url = {https://m2.mtmt.hu/api/publication/31651888}, author = {Krstekanić, N and Matenco, L and Toljić, M and Mandić, O and Stojadinovic, U and Willingshofer, E}, doi = {10.1016/j.gloplacha.2020.103361}, journal-iso = {GLOBAL PLANET CHANGE}, journal = {GLOBAL AND PLANETARY CHANGE}, volume = {195}, unique-id = {31651888}, issn = {0921-8181}, year = {2020}, eissn = {1872-6364} } @article{MTMT:31270514, title = {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}, url = {https://m2.mtmt.hu/api/publication/31270514}, author = {Lukoczki, Georgina and Haas, János and Gregg, JM. and Machel, HG. and Kele, Sándor and John, CM.}, doi = {10.1007/s00531-020-01851-7}, journal-iso = {INT J EARTH SCI}, journal = {INTERNATIONAL JOURNAL OF EARTH SCIENCES}, volume = {109}, unique-id = {31270514}, issn = {1437-3254}, abstract = {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.}, year = {2020}, eissn = {1437-3262}, pages = {1051-1070}, orcid-numbers = {Lukoczki, Georgina/0000-0002-0661-0198; Haas, János/0000-0003-0929-8889; Kele, Sándor/0000-0002-8607-7636} } @article{MTMT:31599438, title = {Syn-sedimentary and early deformation structures as indications for Jurassic pre-orogenic deformation in the SW Bükk Mts.}, url = {https://m2.mtmt.hu/api/publication/31599438}, author = {Oravecz, Éva and Kövér, Szilvia and Héja, Gábor and Fodor, László}, doi = {10.31577/GeolCarp.71.4.3}, journal-iso = {GEOL CARPATH}, journal = {GEOLOGICA CARPATHICA}, volume = {71}, unique-id = {31599438}, issn = {1335-0552}, year = {2020}, eissn = {1336-8052}, pages = {328-342}, orcid-numbers = {Kövér, Szilvia/0000-0002-6736-4226} } @article{MTMT:31044367, title = {Metasomatism-induced wehrlite formation in the upper mantle beneath the Nógrád-Gömör Volcanic Field (Northern Pannonian Basin): Evidence from xenoliths}, url = {https://m2.mtmt.hu/api/publication/31044367}, author = {Patkó, Levente and Liptai, Nóra and Aradi, László Előd and Klébesz, Rita and Sendula, Eszter and Bodnar, Robert J. and Kovács, István János and Hidas, Károly and Cesare, Bernardo and Novák, Attila and Trásy, Balázs and Szabó, Csaba}, doi = {10.1016/j.gsf.2019.09.012}, journal-iso = {GEOSCI FRONT}, journal = {GEOSCIENCE FRONTIERS}, volume = {11}, unique-id = {31044367}, issn = {1674-9871}, year = {2020}, eissn = {1674-9871}, pages = {943-964}, orcid-numbers = {Patkó, Levente/0000-0001-6007-3103; Liptai, Nóra/0000-0002-2464-2468; Aradi, László Előd/0000-0003-0276-3119; Kovács, István János/0000-0002-3488-3716; Szabó, Csaba/0000-0002-1580-6344} } @article{MTMT:31422844, title = {Variable structural styles and tectonic evolution of an ancient backstop boundary: the Pieniny Klippen Belt of the Western Carpathians}, url = {https://m2.mtmt.hu/api/publication/31422844}, author = {Plasienka, Dusan and Bucova, Jana and Simonova, Viera}, doi = {10.1007/s00531-019-01789-5}, journal-iso = {INT J EARTH SCI}, journal = {INTERNATIONAL JOURNAL OF EARTH SCIENCES}, volume = {109}, unique-id = {31422844}, issn = {1437-3254}, abstract = {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.}, keywords = {Cretaceous; Western Carpathians; Paleogene; tectonic evolution; Klippen Belt}, year = {2020}, eissn = {1437-3262}, pages = {1355-1376}, orcid-numbers = {Plasienka, Dusan/0000-0002-7845-4454; Simonova, Viera/0000-0002-7200-0822} } @article{MTMT:31437030, title = {Dawsonite as an indicator of multistage deformation and fluid pathways within fault zones: Insights from the Fore-Dukla Thrust Sheet, Outer Carpathians, Poland}, url = {https://m2.mtmt.hu/api/publication/31437030}, author = {Rybak-Ostrowska, Barbara and Gasinski, Arkadiusz and Kapron, Grzegorz}, doi = {10.24425/agp.2019.126453}, journal-iso = {ACTA GEOL POL}, journal = {ACTA GEOLOGICA POLONICA}, volume = {70}, unique-id = {31437030}, issn = {0001-5709}, abstract = {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.}, keywords = {Fault zone; Outer Carpathians; Syntectonic dawsonite; Multistage development; Fluid pathways}, year = {2020}, eissn = {2300-1887}, pages = {51-78} } @article{MTMT:31646899, title = {RomUkrSeis: Seismic model of the crust and upper mantle across the Eastern Carpathians – From the Apuseni Mountains to the Ukrainian Shield}, url = {https://m2.mtmt.hu/api/publication/31646899}, author = {Starostenko, Vitaly and Janik, Tomasz and Mocanu, Victor and Stephenson, Randell and Yegorova, Tamara and Amashukeli, Tatiana and Czuba, Wojciech and Środa, Piotr and Murovskaya, Anna and Kolomiyets, Katerina and Lysynchuk, Dmytro and Okoń, Jan and Dragut, Alina and Omelchenko, Victor and Legostaieva, Olga and Gryn, Dmytro and Mechie, James and Tolkunov, Anatoly}, doi = {10.1016/j.tecto.2020.228620}, journal-iso = {TECTONOPHYSICS}, journal = {TECTONOPHYSICS}, volume = {794}, unique-id = {31646899}, issn = {0040-1951}, year = {2020}, eissn = {1879-3266}, pages = {1-28} } @article{MTMT:30626415, title = {Palynology and weathering proxies reveal climatic fluctuations during the Carnian Pluvial Episode (CPE) (late Triassic) from marine successions in the Transdanubian Range (western Hungary)}, url = {https://m2.mtmt.hu/api/publication/30626415}, author = {Baranyi, Viktória and Rostási, Ágnes and Raucsik, Béla and Kürschner, WM}, doi = {10.1016/j.gloplacha.2019.01.018}, journal-iso = {GLOBAL PLANET CHANGE}, journal = {GLOBAL AND PLANETARY CHANGE}, volume = {177}, unique-id = {30626415}, issn = {0921-8181}, year = {2019}, eissn = {1872-6364}, pages = {157-172}, orcid-numbers = {Baranyi, Viktória/0000-0002-1194-9903; Rostási, Ágnes/0000-0002-0269-390X; Raucsik, Béla/0000-0002-1951-5974} } @article{MTMT:30371245, title = {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}, url = {https://m2.mtmt.hu/api/publication/30371245}, author = {Bónová, Katarína and Bóna, Ján and Pańczyk, Magdalena and Kováčik, Martin and Mikuš, Tomáš and Laurinc, Dušan}, doi = {10.1016/j.palaeo.2018.09.025}, journal-iso = {PALAEOGEOGR PALAEOCL}, journal = {PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY}, volume = {514}, unique-id = {30371245}, issn = {0031-0182}, keywords = {Petrography; Eocene; U–Pb dating; heavy minerals; Magura Basin}, year = {2019}, eissn = {1872-616X}, pages = {768-784} } @article{MTMT:30916695, title = {Present day geokinematics of Central Europe}, url = {https://m2.mtmt.hu/api/publication/30916695}, author = {Caporali, A. and Zurutuza, J. and Bertocco, M. and Ishchenko, M. and Khoda, O.}, doi = {10.1016/j.jog.2019.101652}, journal-iso = {J GEODYN}, journal = {JOURNAL OF GEODYNAMICS}, volume = {132}, unique-id = {30916695}, issn = {0264-3707}, year = {2019} } @article{MTMT:31046757, title = {Calculation of temperature distribution and rheological properties of the lithosphere along transect IV in the Western Carpathian-Pannonian Basin region}, url = {https://m2.mtmt.hu/api/publication/31046757}, author = {Dererova, Jana and Bielik, Miroslav and Kohut, Igor and Godova, Dominika}, doi = {10.2478/congeo-2019-0026}, journal-iso = {CONTRIB GEOPHYS GEODES}, journal = {CONTRIBUTIONS TO GEOPHYSICS AND GEODESY}, volume = {49}, unique-id = {31046757}, issn = {1335-2806}, abstract = {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.}, keywords = {Temperature field; rheological parameters; 2D integrated modelling; compressional and extensional strength; strength envelopes}, year = {2019}, pages = {497-510} } @article{MTMT:30852034, title = {Results, problems and future tasks of palaeostress and fault-slip analyses in the Pannonian Basin: the Hungarian contribution}, url = {https://m2.mtmt.hu/api/publication/30852034}, author = {Fodor, László}, doi = {10.23928/foldt.kozl.2019.149.4.297}, journal-iso = {FÖLDTANI KÖZLÖNY}, journal = {FÖLDTANI KÖZLÖNY}, volume = {149}, unique-id = {30852034}, issn = {0015-542X}, year = {2019}, eissn = {2559-902X}, pages = {297-326} } @article{MTMT:31029211, title = {Deep structure of the Pieniny Klippen Belt in Poland}, url = {https://m2.mtmt.hu/api/publication/31029211}, author = {Golonka, Jan and Pietsch, Kaja and Marzec, Paweł and Kasperska, Monika and Dec, Jerzy and Cichostępski, Kamil and Lasocki, Stanisław}, doi = {10.1007/s00015-019-00345-2}, journal-iso = {SWISS J GEOSCI}, journal = {SWISS JOURNAL OF GEOSCIENCES}, volume = {112}, unique-id = {31029211}, issn = {1661-8726}, year = {2019}, eissn = {1661-8734}, pages = {475-506} } @article{MTMT:30855045, title = {A Kárpát-Pannon térség neogén-kvarter vulkanizmusa és geodinamikai kapcsolata}, url = {https://m2.mtmt.hu/api/publication/30855045}, author = {Harangi, Szabolcs and Haranginé Lukács, Réka}, doi = {10.23928/foldt.kozl.2019.149.3.197}, journal-iso = {FÖLDTANI KÖZLÖNY}, journal = {FÖLDTANI KÖZLÖNY}, volume = {149}, unique-id = {30855045}, issn = {0015-542X}, year = {2019}, eissn = {2559-902X}, pages = {197-232}, orcid-numbers = {Harangi, Szabolcs/0000-0003-2372-4581; Haranginé Lukács, Réka/0000-0002-2338-4209} } @article{MTMT:30350207, title = {Olivine major and trace element compositions coupled with spinel chemistry to unravel the magmatic systems feeding monogenetic basaltic volcanoes}, url = {https://m2.mtmt.hu/api/publication/30350207}, author = {Jankovics, M. Éva and Sági, Tamás and Astbury, R.L. and Petrelli, M. and Kiss, Balázs and Ubide, T. and Németh, Károly and Ntaflos, T. and Harangi, Szabolcs}, doi = {10.1016/j.jvolgeores.2018.11.027}, journal-iso = {J VOLCANOL GEOTH RES}, journal = {JOURNAL OF VOLCANOLOGY AND GEOTHERMAL RESEARCH}, volume = {369}, unique-id = {30350207}, issn = {0377-0273}, year = {2019}, eissn = {1872-6097}, pages = {203-223}, orcid-numbers = {Jankovics, M. Éva/0000-0001-7079-4422; Sági, Tamás/0000-0003-4664-5472; Kiss, Balázs/0000-0003-0040-0656; Harangi, Szabolcs/0000-0003-2372-4581} } @article{MTMT:30738360, title = {Moho depth analysis of the eastern Pannonian Basin and the Southern Carpathians from receiver functions}, url = {https://m2.mtmt.hu/api/publication/30738360}, author = {Kalmár, Dániel and Hetényi, György and Bondár, István}, doi = {10.1007/s10950-019-09847-w}, journal-iso = {J SEISMOL}, journal = {JOURNAL OF SEISMOLOGY}, volume = {23}, unique-id = {30738360}, issn = {1383-4649}, year = {2019}, eissn = {1573-157X}, pages = {967-982}, orcid-numbers = {Hetényi, György/0000-0001-9036-4761; Bondár, István/0000-0002-4892-1074} } @article{MTMT:30727878, title = {Noble gas and carbon isotope systematics at the seemingly inactive Ciomadul volcano (Eastern‐Central Europe, Romania): evidence for volcanic degassing}, url = {https://m2.mtmt.hu/api/publication/30727878}, author = {Kis, Boglárka Mercédesz and Caracausi, A. and Palcsu, László and Baciu, C. and Ionescu, Artur and Futó, István and Sciarra, A. and Harangi, Szabolcs}, doi = {10.1029/2018GC008153}, journal-iso = {GEOCHEM GEOPHY GEOSY}, journal = {GEOCHEMISTRY GEOPHYSICS GEOSYSTEMS}, volume = {20}, unique-id = {30727878}, year = {2019}, eissn = {1525-2027}, pages = {3019-3043}, orcid-numbers = {Kis, Boglárka Mercédesz/0000-0003-4458-1639; Caracausi, A./0000-0003-2510-2890; Palcsu, László/0000-0002-6542-7537; Sciarra, A./0000-0003-3767-3105; Harangi, Szabolcs/0000-0003-2372-4581} } @article{MTMT:30850025, title = {A földköpeny reológiai kutatása: mennyiségi Fourier transzformációs infravörös spektrometria alkalmazása egy Persány hegységi xenolit példáján}, url = {https://m2.mtmt.hu/api/publication/30850025}, author = {Lange, Thomas Pieter and Szabó, Csaba and Liptai, Nóra and Patkó, Levente and Gelencsér, Orsolya and Aradi, László Előd and Kovács, István János}, doi = {10.23928/foldt.kozl.2019.149.3.233}, journal-iso = {FÖLDTANI KÖZLÖNY}, journal = {FÖLDTANI KÖZLÖNY}, volume = {149}, unique-id = {30850025}, issn = {0015-542X}, year = {2019}, eissn = {2559-902X}, pages = {233-254}, orcid-numbers = {Lange, Thomas Pieter/0000-0002-8709-9239; Szabó, Csaba/0000-0002-1580-6344; Liptai, Nóra/0000-0002-2464-2468; Patkó, Levente/0000-0001-6007-3103; Gelencsér, Orsolya/0000-0001-8615-9298; Aradi, László Előd/0000-0003-0276-3119; Kovács, István János/0000-0002-3488-3716} } @article{MTMT:30415355, title = {Smectite appearance in the footwall of the Úrkút manganese ore deposit, Bakony Mts., Hungary}, url = {https://m2.mtmt.hu/api/publication/30415355}, author = {Leskó, Máté Zsigmond and Papp, Richárd Zoltán and Topa, Boglárka Anna and Kristály, Ferenc and Vigh, Tamás and Zajzon, Norbert}, doi = {10.1556/24.62.2019.02}, journal-iso = {CENT EUR GEOL}, journal = {CENTRAL EUROPEAN GEOLOGY}, volume = {62}, unique-id = {30415355}, issn = {1788-2281}, year = {2019}, eissn = {1789-3348}, pages = {100-118}, orcid-numbers = {Topa, Boglárka Anna/0000-0003-1996-2261; Kristály, Ferenc/0000-0002-0075-5994} } @article{MTMT:30706849, title = {Lateral and vertical heterogeneity in the lithospheric mantle at the northern margin of the Pannonian Basin reconstructed from peridotite xenolith microstructures}, url = {https://m2.mtmt.hu/api/publication/30706849}, author = {Liptai, Nóra and Hidas, K. and Tommasi, A. and Patkó, Levente and Kovács, István János and Griffin, W.L. and O'Reilly, S.Y. and Pearson, N.J. and Szabó, Csaba}, doi = {10.1029/2018JB016582}, journal-iso = {J GEOPHYS RES SOLID EARTH}, journal = {JOURNAL OF GEOPHYSICAL RESEARCH: SOLID EARTH}, volume = {124}, unique-id = {30706849}, issn = {2169-9313}, year = {2019}, eissn = {2169-9356}, pages = {6315-6336}, orcid-numbers = {Liptai, Nóra/0000-0002-2464-2468; Hidas, K./0000-0003-1371-0362; Patkó, Levente/0000-0001-6007-3103; Kovács, István János/0000-0002-3488-3716; O'Reilly, S.Y./0000-0002-3883-5498; Szabó, Csaba/0000-0002-1580-6344} } @article{MTMT:30797506, title = {The intramontane Orava Basin - evidence of large-scale Miocene to Quaternary sinistral wrenching in the Alpine-Carpathian-Pannonian area}, url = {https://m2.mtmt.hu/api/publication/30797506}, author = {Ludwiniak, Miroslaw and Smigielski, Michal and Kowalczyk, Sebastian and Lozinski, Maciej and Czarniecka, Urszula and Lewinska, Lena}, doi = {10.24425/agp.2019.126449}, journal-iso = {ACTA GEOL POL}, journal = {ACTA GEOLOGICA POLONICA}, volume = {69}, unique-id = {30797506}, issn = {0001-5709}, keywords = {Western Carpathians; Structural analysis; Orava Basin; Central Carpathian Palaeogene Basin; Strike-slip related basin; Transrotational basin; Joint pattern analysis}, year = {2019}, eissn = {2300-1887}, pages = {339-386} } @article{MTMT:30342399, title = {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}, url = {https://m2.mtmt.hu/api/publication/30342399}, author = {Lukoczki, Georgina and Haas, János and Gregg, JM and Machel, HG and Kele, Sándor and John, CM}, doi = {10.1016/j.marpetgeo.2018.12.004}, journal-iso = {MAR PETROL GEOL}, journal = {MARINE AND PETROLEUM GEOLOGY}, volume = {101}, unique-id = {30342399}, issn = {0264-8172}, keywords = {Stable Isotope; palaeogeography; Middle Triassic; Mecsek Mts.; dolomitization; clumped isotope}, year = {2019}, eissn = {1873-4073}, pages = {440-458}, orcid-numbers = {Lukoczki, Georgina/0000-0002-0661-0198; Haas, János/0000-0003-0929-8889; Kele, Sándor/0000-0002-8607-7636; John, CM/0000-0001-9711-1548} } @article{MTMT:3240055, title = {Confined carbonates–Regional scale hydraulic interaction or isolation?}, url = {https://m2.mtmt.hu/api/publication/3240055}, author = {Mádlné Szőnyi, Judit and Czauner, Brigitta and Iván, Veronika and Tóth, Ádám and Simon, Szilvia and Erőss, Anita and Kovácsné Bodor, Petra and Trásy-Havril, Tímea and Boncz, László and Sőreg, Viktor}, doi = {10.1016/j.marpetgeo.2017.06.006}, journal-iso = {MAR PETROL GEOL}, journal = {MARINE AND PETROLEUM GEOLOGY}, volume = {107}, unique-id = {3240055}, issn = {0264-8172}, year = {2019}, eissn = {1873-4073}, pages = {591-612}, orcid-numbers = {Mádlné Szőnyi, Judit/0000-0002-5628-4386; Czauner, Brigitta/0000-0001-6591-8611; Tóth, Ádám/0000-0002-7300-6687; Simon, Szilvia/0000-0002-3811-9141; Erőss, Anita/0000-0002-2395-3934; Trásy-Havril, Tímea/0000-0003-3478-2787} } @article{MTMT:30658244, title = {Provenance and Variscan low-grade regional metamorphism recorded in slates from the basement of the (SW Hungary)}, url = {https://m2.mtmt.hu/api/publication/30658244}, author = {Mészáros, Előd and Raucsikné Varga, Andrea Beáta and Raucsik, Béla and Benkó, Zsolt and Heincz, Adrián László and Hauzenberger, CA}, doi = {10.1007/s00531-019-01720-y}, journal-iso = {INT J EARTH SCI}, journal = {INTERNATIONAL JOURNAL OF EARTH SCIENCES}, volume = {108}, unique-id = {30658244}, issn = {1437-3254}, year = {2019}, eissn = {1437-3262}, pages = {1571-1593}, orcid-numbers = {Mészáros, Előd/0000-0002-5846-9034; Raucsikné Varga, Andrea Beáta/0000-0002-8673-1482; Raucsik, Béla/0000-0002-1951-5974; Heincz, Adrián László/0000-0001-7563-0136} } @article{MTMT:30642272, title = {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}, url = {https://m2.mtmt.hu/api/publication/30642272}, author = {Patkó, Levente and Liptai, Nóra and Kovács, István János and Aradi, László Előd and Xia, Q.-K. and Ingrin, J. and Mihály, Judith and O'Reilly, S.Y. and Griffin, W.L. and Wesztergom, Viktor and Szabó, Csaba}, doi = {10.1016/j.chemgeo.2018.12.017}, journal-iso = {CHEM GEOL}, journal = {CHEMICAL GEOLOGY}, volume = {507}, unique-id = {30642272}, issn = {0009-2541}, year = {2019}, eissn = {1872-6836}, pages = {23-41}, orcid-numbers = {Patkó, Levente/0000-0001-6007-3103; Liptai, Nóra/0000-0002-2464-2468; Kovács, István János/0000-0002-3488-3716; Aradi, László Előd/0000-0003-0276-3119; Szabó, Csaba/0000-0002-1580-6344} } @article{MTMT:30321155, title = {Variation in style of magmatism and emplacement mechanism induced by changes in basin environments and stress fields (Pannonian Basin, Central Europe)}, url = {https://m2.mtmt.hu/api/publication/30321155}, author = {Petrik, Attila and Fodor, László and Bereczki, László and Klembala, Zs and Haranginé Lukács, Réka and Baranyi, Viktória and Beke, Barbara and Harangi, Szabolcs}, doi = {10.1111/bre.12326}, journal-iso = {BASIN RES}, journal = {BASIN RESEARCH}, volume = {31}, unique-id = {30321155}, issn = {0950-091X}, year = {2019}, eissn = {1365-2117}, pages = {380-404}, orcid-numbers = {Haranginé Lukács, Réka/0000-0002-2338-4209; Baranyi, Viktória/0000-0002-1194-9903; Beke, Barbara/0000-0003-0797-1195; Harangi, Szabolcs/0000-0003-2372-4581} } @article{MTMT:30802650, title = {Tectonic units of the Alpine collision zone between Eastern Alps and western Turkey}, url = {https://m2.mtmt.hu/api/publication/30802650}, author = {Schmid, SM. and Fügenschuh, B and Kounov, A and Matenco, L and Nievergelt, P and Oberhänsli, R and Pleuger, J and Schefer, S and Schuster, R and Tomljenović, B and Ustaszewski, K and van Hinsbergen, DJJ.}, doi = {10.1016/j.gr.2019.07.005}, journal-iso = {GONDWANA RES}, journal = {GONDWANA RESEARCH}, volume = {78}, unique-id = {30802650}, issn = {1342-937X}, year = {2019}, eissn = {1878-0571}, pages = {308-374} } @article{MTMT:30388038, title = {Continental lithospheric structure from the East European Craton to the Pannonian Basin based on integrated geophysical modelling}, url = {https://m2.mtmt.hu/api/publication/30388038}, author = {Šimonová, Barbora and Zeyen, Hermann and Bielik, Miroslav}, doi = {10.1016/j.tecto.2018.12.003}, journal-iso = {TECTONOPHYSICS}, journal = {TECTONOPHYSICS}, volume = {750}, unique-id = {30388038}, issn = {0040-1951}, year = {2019}, eissn = {1879-3266}, pages = {289-300} } @article{MTMT:3399845, title = {Pervasive early diagenetic dolomitization, subsequent hydrothermal alteration, and late stage hydrocarbon accumulation in a Middle Triassic carbonate sequence (Szeged Basin, SE Hungary)}, url = {https://m2.mtmt.hu/api/publication/3399845}, author = {Garaguly, István and Raucsikné Varga, Andrea Beáta and Raucsik, Béla and Schubert, Félix and Czuppon, György and Frei, R}, doi = {10.1016/j.marpetgeo.2018.07.024}, journal-iso = {MAR PETROL GEOL}, journal = {MARINE AND PETROLEUM GEOLOGY}, volume = {98}, unique-id = {3399845}, issn = {0264-8172}, year = {2018}, eissn = {1873-4073}, pages = {270-290}, orcid-numbers = {Garaguly, István/0000-0002-2802-0738; Raucsikné Varga, Andrea Beáta/0000-0002-8673-1482; Raucsik, Béla/0000-0002-1951-5974; Schubert, Félix/0000-0001-8647-5354; Czuppon, György/0000-0002-7231-6042} } @article{MTMT:30430761, title = {The deepest Moho in the Western Carpathians and its respective crustal density model (CEL12 section)}, url = {https://m2.mtmt.hu/api/publication/30430761}, author = {Godova, Dominika and Bielik, Miroslav and Simonova, Barbora}, doi = {10.2478/congeo-2018-0011}, journal-iso = {CONTRIB GEOPHYS GEODES}, journal = {CONTRIBUTIONS TO GEOPHYSICS AND GEODESY}, volume = {48}, unique-id = {30430761}, issn = {1335-2806}, keywords = {gravimetry; density modelling; seismic constraints; External Western Carpathians Flysch zone; CELEBRATION; Bouguer gravity}, year = {2018}, pages = {255-269} } @article{MTMT:30321138, title = {Geochronology of granitoids from Psunj and Papuk Mts., Croatia}, url = {https://m2.mtmt.hu/api/publication/30321138}, author = {Horvat, M. and Klötzli, U. and Jamičić, D. and Buda, György and Klötzli, E. and Hauzenberger, C.}, doi = {10.1515/geochr-2015-0099}, journal-iso = {GEOCHRONOMETRIA}, journal = {GEOCHRONOMETRIA}, volume = {45}, unique-id = {30321138}, issn = {1733-8387}, abstract = {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.}, keywords = {MODEL; EVOLUTION; Pannonian Basin; METAMORPHISM; U-PB; ZIRCON GEOCHRONOLOGY; monzogranite; Late Devonian; Psunj Mt.; Papuk Mt.; Geosciences, Multidisciplinary; TISIA MEGA-UNIT; SLAVONIAN MOUNTAINS; SOUTH TISIA; NE CROATIA}, year = {2018}, eissn = {1897-1695}, pages = {198-210} } @article{MTMT:30432320, title = {Miocene paleogeography and biostratigraphy of the Slovenj Gradec Basin: a marine corridor between the Mediterranean and Central Paratethys}, url = {https://m2.mtmt.hu/api/publication/30432320}, author = {Ivancic, Kristina and Trajanova, Mirka and Coric, Stjepan and Rozic, Bostjan and Smuc, Andrej}, doi = {10.1515/geoca-2018-0031}, journal-iso = {GEOL CARPATH}, journal = {GEOLOGICA CARPATHICA}, volume = {69}, unique-id = {30432320}, issn = {1335-0552}, keywords = {biostratigraphy; Miocene; Sequence stratigraphy; paleogeography; CENTRAL PARATETHYS; PANNONIAN BASIN SYSTEM; Slovenj Gradec Basin}, year = {2018}, eissn = {1336-8052}, pages = {528-544} } @article{MTMT:30479664, title = {Ultrasonic constraint of the microfracture anisotropy of flysch rocks from the Podhale Synclinorium (Poland)}, url = {https://m2.mtmt.hu/api/publication/30479664}, author = {Kopotowska, Agnieszka}, doi = {10.1007/s00531-017-1579-1}, journal-iso = {INT J EARTH SCI}, journal = {INTERNATIONAL JOURNAL OF EARTH SCIENCES}, volume = {107}, unique-id = {30479664}, issn = {1437-3254}, abstract = {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.}, keywords = {Joints; Ultrasonic Waves; Microfractures; Flysch rocks; Dynamic elastic properties}, year = {2018}, eissn = {1437-3262}, pages = {1941-1953} } @article{MTMT:27587223, title = {Changes in Cenozoic depositional environment and sediment provenance in the Danube Basin}, url = {https://m2.mtmt.hu/api/publication/27587223}, author = {Kovac, M and Rybar, S and Halasova, E and Hudackova, N and Sarinova, K and Sujan, M and Baranyi, Viktória and Kovacova, M and Ruman, A and Kluciar, T and Zlinska, A}, doi = {10.1111/bre.12244}, journal-iso = {BASIN RES}, journal = {BASIN RESEARCH}, volume = {30}, unique-id = {27587223}, issn = {0950-091X}, year = {2018}, eissn = {1365-2117}, pages = {97-131}, orcid-numbers = {Sujan, M/0000-0001-7933-8669; Baranyi, Viktória/0000-0002-1194-9903} } @article{MTMT:3391954, title = {Miocene basin opening in relation to the north-eastward tectonic extrusion of the ALCAPA Mega-Unit}, url = {https://m2.mtmt.hu/api/publication/3391954}, author = {Kovac, M and Márton Péterné Szalay, Emőke and Kluciar, T and Vojtko, R}, doi = {10.1515/geoca-2018-0015}, journal-iso = {GEOL CARPATH}, journal = {GEOLOGICA CARPATHICA}, volume = {69}, unique-id = {3391954}, issn = {1335-0552}, abstract = {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.}, keywords = {Pannonian Basin; Neogene; Eastern Alps; Danube Basin; Lateral extrusion; STRUCTURAL EVOLUTION; basin development; ADJOINING AREAS; DEPOSITIONAL SYSTEMS; COUNTERCLOCKWISE ROTATION; STRESS-FIELD EVOLUTION; CENTRAL-WESTERN CARPATHIANS; "en block and domino-effect" counter-clockwise rotations; ALCAPA Mega-Unit}, year = {2018}, eissn = {1336-8052}, pages = {254-263}, orcid-numbers = {Márton Péterné Szalay, Emőke/0000-0002-2135-8867} } @article{MTMT:30479651, title = {Basin modelling with a MATLAB-based program, BasinVis 2.0: A case study on the southern Vienna Basin, Austria}, url = {https://m2.mtmt.hu/api/publication/30479651}, author = {Lee, Eun Young and Wagreich, Michael}, doi = {10.14770/jgsk.2018.54.6.615}, journal-iso = {J GEO SOC KOREA}, journal = {JOURNAL OF THE GEOLOGICAL SOCIETY OF KOREA}, volume = {54}, unique-id = {30479651}, issn = {0435-4036}, abstract = {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.}, keywords = {Vienna Basin; basin analysis; subsidence; BasinVis 2.0; basin modelling}, year = {2018}, eissn = {2288-7377}, pages = {615-630} } @article{MTMT:3339119, title = {Early to Mid-Miocene syn-extensional massive silicic volcanism in the Pannonian Basin (East-Central Europe): Eruption chronology, correlation potential and geodynamic implications}, url = {https://m2.mtmt.hu/api/publication/3339119}, author = {Haranginé Lukács, Réka and Harangi, Szabolcs and Guillong, M and Bachmann, O and Fodor, László and Buret, Y and Dunkl, István and Sliwinski, J and von Quadt, A and Peytcheva, I and Zimmerer, M}, doi = {10.1016/j.earscirev.2018.02.005}, journal-iso = {EARTH-SCI REV}, journal = {EARTH-SCIENCE REVIEWS}, volume = {179}, unique-id = {3339119}, issn = {0012-8252}, abstract = {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).}, keywords = {NEW-ZEALAND; Pannonian Basin; Bükkalja volcanic field; Bükkalja volcanic field; LA-ICP-MS; tectonic evolution; Paratethys; U-PB; Back-arc basins; CENTRAL ANDES; structural control; INTRA-CARPATHIAN AREA; Eruption chronology; syn-extensional volcanism; Silicic ignimbrite; LONG VALLEY CALDERA; SOUTHERN GREAT-BASIN; Zircon ages; Zircon ages}, year = {2018}, eissn = {1872-6828}, pages = {1-19}, orcid-numbers = {Haranginé Lukács, Réka/0000-0002-2338-4209; Harangi, Szabolcs/0000-0003-2372-4581} } @article{MTMT:3360352, title = {The onset of the volcanism in the Ciomadul Volcanic Dome Complex (Eastern Carpathians): Eruption chronology and magma type variation}, url = {https://m2.mtmt.hu/api/publication/3360352}, author = {Molnár, Kata and Harangi, Szabolcs and Haranginé Lukács, Réka and Dunkl, István and Schmitt, AK and Kiss, Balázs and Garamhegyi, Tamás and Seghedi, I}, doi = {10.1016/j.jvolgeores.2018.01.025}, journal-iso = {J VOLCANOL GEOTH RES}, journal = {JOURNAL OF VOLCANOLOGY AND GEOTHERMAL RESEARCH}, volume = {354}, unique-id = {3360352}, issn = {0377-0273}, abstract = {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.}, keywords = {EVOLUTION; Romania; NEW-ZEALAND; Quaternary; Neogene; Carpathian-Pannonian region; Geochemistry; Central-Europe; U-series dating; Quaternary volcanism; Harghita; PANNONIAN REGION; SE Carpathians; Eruption chronology; Zircon (U-Th)/He dating; ZIRCON GEOCHRONOLOGY}, year = {2018}, eissn = {1872-6097}, pages = {39-56}, orcid-numbers = {Molnár, Kata/0000-0001-6993-5806; Harangi, Szabolcs/0000-0003-2372-4581; Haranginé Lukács, Réka/0000-0002-2338-4209; Kiss, Balázs/0000-0003-0040-0656} } @article{MTMT:27642265, title = {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}, url = {https://m2.mtmt.hu/api/publication/27642265}, author = {Plašienka, D}, doi = {10.1029/2017TC004779}, journal-iso = {TECTONICS}, journal = {TECTONICS}, volume = {37}, unique-id = {27642265}, issn = {0278-7407}, year = {2018}, eissn = {1944-9194}, pages = {2029-2079} } @article{MTMT:27569302, title = {Evolution of the arc-derived orthogneiss recorded in exotic xenoliths of the Koros Complex (Tisza Megaunit, SE Hungary)}, url = {https://m2.mtmt.hu/api/publication/27569302}, author = {M. Tóth, Tivadar and Schubert, Félix}, doi = {10.3190/jgeosci.253}, journal-iso = {J GEOSCI}, journal = {JOURNAL OF GEOSCIENCES}, volume = {63}, unique-id = {27569302}, issn = {1802-6222}, year = {2018}, eissn = {1803-1943}, pages = {21-46}, orcid-numbers = {M. Tóth, Tivadar/0000-0003-1012-1095; Schubert, Félix/0000-0001-8647-5354} } @article{MTMT:3331754, title = {Characterization and DFN modelling of the fracture network in a Mesozoic karst reservoir: Gomba oilfield, Paleogene Basin, Central Hungary}, url = {https://m2.mtmt.hu/api/publication/3331754}, author = {Bauer, Márton and M. Tóth, Tivadar}, doi = {10.1111/jpg.12678}, journal-iso = {J PETROL GEOL}, journal = {JOURNAL OF PETROLEUM GEOLOGY}, volume = {40}, unique-id = {3331754}, issn = {0141-6421}, keywords = {Hungary; Carbonates; FRACTURES; palaeokarst; Gomba field; Paleogene Basin; DFN modelling}, year = {2017}, eissn = {1747-5457}, pages = {319-334}, orcid-numbers = {M. Tóth, Tivadar/0000-0003-1012-1095} } @article{MTMT:27079576, title = {The relationship of the geological framework to the Quaternary aquifer system in the Sava River valley (Croatia)}, url = {https://m2.mtmt.hu/api/publication/27079576}, author = {Brkic, Zeljka}, doi = {10.4154/gc.2017.12}, journal-iso = {GEOL CROAT}, journal = {GEOLOGIA CROATICA}, volume = {70}, unique-id = {27079576}, issn = {1330-030X}, year = {2017}, eissn = {1333-4875}, pages = {201-213} } @article{MTMT:26772395, title = {Slab-derived metasomatism in the Carpathian-Pannonian mantle revealed by investigations of mantle xenoliths from the Bakony-Balaton Highland Volcanic Field}, url = {https://m2.mtmt.hu/api/publication/26772395}, author = {Créon, L and Delpech, G and Rouchon, V and Guyot, F}, doi = {10.1016/j.lithos.2017.06.004}, journal-iso = {LITHOS}, journal = {LITHOS}, volume = {286-287}, unique-id = {26772395}, issn = {0024-4937}, year = {2017}, eissn = {1872-6143}, pages = {534-552} }