@article{MTMT:34538363, title = {Laevaptychi as reliable paleotemperature archives: high-resolution stable isotope compositions of Kimmeridgian (Jurassic) lamellar structured aspidoceratid lower mandibles from Zengővárkony (Mecsek Mountains, Hungary)}, url = {https://m2.mtmt.hu/api/publication/34538363}, author = {Bujtor, László and Demény, Attila and Németh, Péter and Bajnóczi, Bernadett}, doi = {10.1007/s00531-023-02376-5}, journal-iso = {INT J EARTH SCI}, journal = {INTERNATIONAL JOURNAL OF EARTH SCIENCES}, volume = {113}, unique-id = {34538363}, issn = {1437-3254}, abstract = {Fieldwork provided well-preserved Laevaptychus sp. ex gr. hoplisus – obliquus specimens from the lower Kimmeridgian of Zengővárkony (Mecsek Mountains, south Hungary). This study presents the stable isotope analysis of these aptychi and control samples from brachiopods ( Nucleata and Pygope ) derived from the Zengővárkony section bed 3. Rarely observed structures in the upper lamellar layers of the studied laevaptychi revealed 24–32 concentric lamellae that represent primary textural features and indicate excellent preservation. After careful screening for diagenetic effects, stable oxygen isotope compositions yielded seawater temperatures between 20 and 26 °C in good agreement with earlier studies on Jurassic formations, with improved precision. Our research presents for the first time that well-preserved laevaptychi may be a reliable data source for paleoclimate and paleotemperature reconstructions.}, year = {2024}, eissn = {1437-3262}, pages = {353-367}, orcid-numbers = {Bujtor, László/0000-0001-9699-7711; Demény, Attila/0000-0003-0522-9018; Németh, Péter/0000-0001-5592-5877; Bajnóczi, Bernadett/0000-0003-0006-7611} } @article{MTMT:34401167, title = {Continuous wavelet transformation to quantify small-scale cycles of petrophysical properties; a new approach applied in a potential disposal repository of nuclear waste, SW Hungary}, url = {https://m2.mtmt.hu/api/publication/34401167}, author = {Abutaha, Saja and Geiger, János and Fedor, F and Gulyás, Sándor}, doi = {10.4154/gc.2023.11}, journal-iso = {GEOL CROAT}, journal = {GEOLOGIA CROATICA}, volume = {76}, unique-id = {34401167}, issn = {1330-030X}, abstract = {Continuous Wavelet Transformation (CWT) was applied to study the small-scale repetitive oscillations of porosity distribution patterns in a 5 m silty-claystone core sample of the Boda Claystone Formation. We handled the fluctuations in voxel porosity averages over unequal depth distributions as signals over uneven time intervals. The strength of wavelet analysis lies in the ability to study the fluctuation of a signal in detail, i.e., the wavelet transforms permit automatic localization of the cyclic attributes' sequences both in time (the depth domain) and according to their frequency (the frequency domain). Thereupon, three main frequency branches (cycles) were discerned: small scale (5, 6.67, and 11 cm), intermediate scale (20, 30 cm), and large scale (66.67 cm). Depending on the CWT coefficients magnitude plot, we were able to detect the developments of porosity oscillation according to the depth variable. Thus, small-scale cycles were seen throughout the core sample., the intermediate-scale cycles were strong in the upper parts of the core sample and dwindled toward greater depths, and the large cycle was predominant in the lower part of the core sample. The cross-correlation of the wavelet coefficients of porosity and rock-forming components allows a detailed study of the inter-dependence of such parameters as their relationship changes over time. The distinct peaks at zero lag indicates that the measured wavelet coefficient series were contemporaneously correlated; their strong positive correlations suggest that both examined series respond similarly and simultaneously to other exogenous factors. The results emphasize that cyclical porosity fluctuations at all scales would concern three main factors; sediment deposition, diagenetic processes, and structural deformation (i.e., convolute laminations).}, year = {2023}, eissn = {1333-4875}, pages = {131-146}, orcid-numbers = {Abutaha, Saja/0000-0001-8439-5895; Geiger, János/0000-0001-9359-5266; Gulyás, Sándor/0000-0002-3384-2381} } @article{MTMT:33727168, title = {Interpretation of wide zircon U–Pb age distributions in durbachite-type Variscan granitoid in the Mórágy Hills}, url = {https://m2.mtmt.hu/api/publication/33727168}, author = {Kis, Annamária and Weiszburg, Tamás and Dunkl, István and Koller, F. and Váczi, Tamás and Buda, György}, doi = {10.1007/s00710-023-00817-2}, journal-iso = {MINER PETROL}, journal = {MINERALOGY AND PETROLOGY}, volume = {117}, unique-id = {33727168}, issn = {0930-0708}, year = {2023}, eissn = {1438-1168}, pages = {663-683}, orcid-numbers = {Weiszburg, Tamás/0000-0001-8183-4434; Váczi, Tamás/0000-0003-0142-545X} } @article{MTMT:34057402, title = {Chronostratigraphic overview of the Toarcian (Early Jurassic) ammonite fauna from the Mecsek Mountains (Hungary)}, url = {https://m2.mtmt.hu/api/publication/34057402}, author = {Kovács, Z and Horváth-Kostka, Zsófia Rita and Müller, Tamás and Pálfy, József}, doi = {10.31577/GeolCarp.2023.14}, journal-iso = {GEOL CARPATH}, journal = {GEOLOGICA CARPATHICA}, volume = {74}, unique-id = {34057402}, issn = {1335-0552}, keywords = {Toarcian; Chronostratigraphy; Mecsek Mountains; PALEOBIOGEOGRAPHY; Early Jurassic; Ammonitina}, year = {2023}, eissn = {1336-8052}, pages = {211-232}, orcid-numbers = {Kovács, Z/0000-0001-7276-7321; Pálfy, József/0000-0001-9686-1849} } @article{MTMT:34500255, title = {Tracing the latest Jurassic-earliest Cretaceous paleoenvironment evolution in swell carbonate facies: a case study of the High-Tatric succession (Central Western Carpathians, Tatra Mts, Poland)}, url = {https://m2.mtmt.hu/api/publication/34500255}, author = {Lodowski, D.G. and Grabowski, J.}, doi = {10.24425/agp.2023.145629}, journal-iso = {ACTA GEOL POL}, journal = {ACTA GEOLOGICA POLONICA}, volume = {73}, unique-id = {34500255}, issn = {0001-5709}, year = {2023}, eissn = {2300-1887}, pages = {741-772} } @article{MTMT:33842343, title = {The Lower Cretaceous Carpatho-Cimmerian bioprovince: The contribution of rudist bivalves (Hippuritida)}, url = {https://m2.mtmt.hu/api/publication/33842343}, author = {Masse, Jean-Pierre and Fenerci-Masse, Mukerrem and Bucur, Ioan I.}, doi = {10.1016/j.cretres.2022.105448}, journal-iso = {CRETACEOUS RES}, journal = {CRETACEOUS RESEARCH}, volume = {144}, unique-id = {33842343}, issn = {0195-6671}, abstract = {The Carpatho-Cimmerian bioprovince is a Barremian-lower Aptian entity. Its definition based on the coexistence of two calcareous algae and a foraminifera, is well supported by a distinctive rudist assemblage. Thirteen species: Requienia zlatarskii, Lovetchenia lovetchensis, Lovetchenia drinovi, Love-tchenia stratechi, Toucasia petersi, Parapachytraga gigantea, Paragyropleura paquieri, Debrunia ? dibrariana, Debrunia ? kafanensis, Homopleura balkanica, Homopleura ? minima, Homopleura? gigantea and Bicor-nucopina petersi are characteristic, endemic members of this bioprovince. The Carpatho-Cimmerian bioprovince shared some taxa with Western Europe and Apulian biomes. The Carpatho-Cimmerian rudist assemblage extends from Hungary, Romania, Bulgaria, Slovakia, Ukraine, Southern Russia, Northern Turkey, Armenia, Azerbaidjan and probably Turkmenistan. The South Bohemian shelfal discontinuity between the Western European and the Balkanic regions, accounts well for the dissimi-larity of the corresponding faunas.(c) 2022 Elsevier Ltd. All rights reserved.}, keywords = {Lower Cretaceous; Rudists; Barremian-lower Aptian; Carpatho-Cimmerian}, year = {2023}, eissn = {1095-998X} } @article{MTMT:33656335, title = {Tracing the cryptic Sardic (Ordovician) metamorphism across Alpine Europe: the Krndija region in the Slavonian Mountains, Croatia}, url = {https://m2.mtmt.hu/api/publication/33656335}, author = {Mayer, B.S. and Zeh, A. and Krenn, E. and Gerdes, A. and Finger, F.}, doi = {10.1007/s00531-022-02282-2}, journal-iso = {INT J EARTH SCI}, journal = {INTERNATIONAL JOURNAL OF EARTH SCIENCES}, unique-id = {33656335}, issn = {1437-3254}, year = {2023}, eissn = {1437-3262} } @article{MTMT:34069281, title = {Did the Western and the Eastern Vardar ophiolites originate through a single intra-oceanic subduction? Insight from numerical modelling}, url = {https://m2.mtmt.hu/api/publication/34069281}, author = {Stanković, Nikola and Gerya, Taras and Cvetkov, Vesna and Cvetković, Vladica}, doi = {10.1016/j.gr.2023.07.005}, journal-iso = {GONDWANA RES}, journal = {GONDWANA RESEARCH}, volume = {124}, unique-id = {34069281}, issn = {1342-937X}, year = {2023}, eissn = {1878-0571}, pages = {124-140}, orcid-numbers = {Stanković, Nikola/0000-0003-4151-4414; Cvetkov, Vesna/0000-0002-3596-0306} } @article{MTMT:33594461, title = {Revealing the Mineralogical and Petrographic Signs of Fluid-Related Processes in the Kelebia Basement Area (Szeged Basin, S Hungary): A Case Study of Alpine Prograde Metamorphism in a Permo-Triassic Succession}, url = {https://m2.mtmt.hu/api/publication/33594461}, author = {Raucsikné Varga, Andrea Beáta and Pál-Molnár, Elemér and Raucsik, Béla}, doi = {10.1155/2023/8600576}, journal-iso = {GEOFLUIDS}, journal = {GEOFLUIDS}, volume = {2023}, unique-id = {33594461}, issn = {1468-8115}, abstract = {The Szeged Basin (S Hungary) occupies a relatively central position within the European Alpine–Carpathian–Dinaride orogenic belt. An ongoing controversy about the tectonic position of the study area indicates that its evolution is still not fully understood; however, several important hydrocarbon occurrences are known in the fractured basement reservoirs. The main aim of this contribution is to investigate the petrographic features and possible Alpine metamorphic conditions of volcanic/volcanoclastic and siliciclastic rocks from the Kelebia basement area. Due to the outcrop conditions and poor exposure, study samples are obtained from cores and core chips resulting from oil exploration. Based on an evaluation of petrographic (including also cathodoluminescence analysis) and microstructural features, joined with mineralogical and metamorphic data such as “illite crystallinity” and K-white mica crystallite size obtained by X-ray powder diffractometry (XRPD), a very low- to low-grade (ca. 300°C) Alpine metamorphic imprint of this portion of the basement can be proposed. Several deformation characteristics (deformation lamellae in quartz, deformation twins in dolomite, fragmented porphyroclasts, and strain shadows) were recognized in the studied samples, showing a weakly to moderately developed disjunctive foliation in the Permian rocks, as well as quartz veinlets, microcracks, and fluid inclusion planes in the Lower Triassic sandstones. Most likely, one of the Cretaceous orogenic events, namely, the “Turonian” phase (Early–Late Cretaceous nappe stacking), resulted in the prograde greenschist facies metamorphism in the study area, instead of the burial depth. We propose that the Permo-Triassic cover succession was also affected by shearing episodes accompanied by fluid migrations along the contact zone between the tectonic units. The scientific approach and dataset provided here are examples of how the application of XRPD parameters of phyllosilicates and micropetrographic observations can help to understand the evolution of an orogen and improve knowledge about the basement structure.}, year = {2023}, eissn = {1468-8123}, pages = {1-18}, orcid-numbers = {Raucsikné Varga, Andrea Beáta/0000-0002-8673-1482; Pál-Molnár, Elemér/0000-0002-9606-0133; Raucsik, Béla/0000-0002-1951-5974} } @article{MTMT:33219431, title = {Middle Triassic (Anisian) Cephalopods From the Mecsek Mountains, Hungary}, url = {https://m2.mtmt.hu/api/publication/33219431}, author = {Vörös, Attila and Konrád, Gyula and Sebe, Krisztina}, doi = {10.54103/2039-4942/17253}, journal-iso = {RIV IT PALEON STRATIG}, journal = {RIVISTA ITALIANA DI PALEONTOLOGIA E STRATIGRAFIA}, volume = {128}, unique-id = {33219431}, issn = {0035-6883}, abstract = {Recent nautiloid and ammonoid finds from the Middle Triassic Zuhánya Limestone Formation in the Mecsek Mountains (south Hungary) proved that the formation encompasses the whole Pelsonian and the lower Illyrian substages of the Anisian Stage. On the basis of 11 identified ammonoid species, the Balatonicus and Trinodosus zones have a complete record. The stratigraphical position of the Zuhánya Limestone on the whole corresponds to the Felsőörs Limestone in the Balaton Highland. The palaeobiogeographical evaluation of the cephalopod fauna showed that the elements of the nautilid fauna point mostly to Germanic and partly to Sephardic affinity. On the other hand, the ammonoid fauna has no Germanic elements; most of the species are Alpine in character, while the species Procladiscites brancoi indicates Dinaridic connection, or at least an occasional appearance of pelagic organisms. These results endorse the previous palaeogeographical assumption and suggest that during the Middle Triassic the Mecsek succession was situated along the European shelf, between the Vindelician-Bohemian Land and the open Tethyan Ocean.}, year = {2022}, eissn = {2039-4942}, pages = {695-717}, orcid-numbers = {Sebe, Krisztina/0000-0002-4647-2199} } @article{MTMT:32589010, title = {Evaluation of 3D small-scale lithological heterogeneities and pore distribution of the Boda Claystone Formation using X-Ray Computed Tomography images (CT)}, url = {https://m2.mtmt.hu/api/publication/32589010}, author = {Abutaha, Saja and Geiger, János and Gulyás, Sándor and Fedor, Ferenc}, doi = {10.4154/gc.2021.17}, journal-iso = {GEOL CROAT}, journal = {GEOLOGIA CROATICA}, volume = {74}, unique-id = {32589010}, issn = {1330-030X}, year = {2021}, eissn = {1333-4875}, pages = {305-318}, orcid-numbers = {Abutaha, Saja/0000-0001-8439-5895; Geiger, János/0000-0001-9359-5266; Gulyás, Sándor/0000-0002-3384-2381} } @article{MTMT:31792001, title = {Fauna, palaeoecology and ecotypes of the Early Cretaceous sediment hosted hydrothermal vent environment of Zengővárkony (Mecsek Mountains, Hungary)}, url = {https://m2.mtmt.hu/api/publication/31792001}, author = {Bujtor, László and Nagy, J}, doi = {10.1016/j.palaeo.2020.110179}, journal-iso = {PALAEOGEOGR PALAEOCL}, journal = {PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY}, volume = {564}, unique-id = {31792001}, issn = {0031-0182}, abstract = {The fossil biota of the upper Valanginian–lower Hauterivian sediment hosted vent (SHV) environment of Zeng ˝ov´arkony comprises 39 species, 55 genera and higher taxa representing seven phyla. Thirteen of these taxa are reported from Zeng˝orv´arkony as new species or new subgenera/genera, and this high endemicity is linked to a unique palaeoenvironment. The palaeoenvironment is developed in an outer shelf epicontinental setting on an elevated block or slope, and is linked to a small sedimentary iron-ore body interbedded with pillow lavas being a result of ferriferous exhalations and biogenic processes. Biogeographically, the brachiopods indicate the Sub- Tethyan domain. Serial sectioning of brachiopods revealed a taxon-dependent rich and diverse microfauna (sponges, foraminifers, gastropods) preserved inside the shells. Internally preserved microfauna in brachiopods reveals differentiation among preventive strategies. It implies different preventive efficiencies of alternative defence strategies of higher brachiopod taxa. The unique Zeng˝ov´arkony SHV environment attracted both nektonic and benthic organisms by creating different ecotopes around the hydrothermally driven bottom environment. This environment belongs to the group of rare, shelfal, hydrothermally influenced palaeoenvironments formed on continental crust. Water depth was most probably between 100 and 150 m. Recent observations from a similar modern volcanic built-up, and its effects on the marine environment located on continental crust around the Aeolian Islands (Tyrrhenian Sea) support the recognition of this fossil SHV environment and helps to understand better its bathymetry, ecological conditions and ore-formation.}, year = {2021}, eissn = {1872-616X}, orcid-numbers = {Bujtor, László/0000-0001-9699-7711} } @article{MTMT:32090766, title = {Kimmeridgian and early Tithonian cephalopods from the Kisújbánya Limestone Formation, Zengővárkony (Mecsek Mountains, southern Hungary), their faunal composition, palaeobiogeographic affinities, and taphonomic character}, url = {https://m2.mtmt.hu/api/publication/32090766}, author = {Bujtor, László and Albrecht, Richárd Gyula and Farkas, Csaba and Makó, B and Maróti, D and Miklósy, Á}, doi = {10.2110/carnets.2021.2113}, journal-iso = {CARNETS GEOL}, journal = {CARNETS DE GEOLOGIE}, volume = {21}, unique-id = {32090766}, issn = {1765-2553}, abstract = {A new collection at Zengővárkony (Mecsek Mountains, Hungary) provided a rich and diverse but poorly preserved cephalopod-dominated fossil assemblage representing the Kimmeridgian and the lower Tithonian. The material came from mixed scree, soil, and amongst roots affected by weathering processes having been exposed to the elements for a long time. The nautiloid Pseudaganides strambergensis is the first record from the Mecsek Mountains. Due to the weathering, the ammonite fauna consists of mainly fragmentary and dissolved individuals that comprises 528 specimens belonging to 34 species and 30 genera out of which 20 species and 15 genera are reported for the first time from the Mecsek Mountains. The fauna includes specimens of known taxa. No new taxa are introduced. Based on the comparison with other faunas, this assemblage most closely resembles the fauna of the Venetian Alps (Italy). Additional faunal elements include aptychi (Laevaptychus latus, Lamellaptychus murocostatus), belemnites (Hibolithes semisulcatus), and an indetermined brachiopod. The first record of Spiraserpula spirolinites, an encrusting fossil polychaete preserved on the internal mould of a Taramelliceras shell fragment indicates favourable bottom conditions for the epifauna. The presence of Aspidoceras caletanum, Gravesia aff. gigas, and Pseudowaagenia inerme indicates faunal connections with the Submediterranean Province of the Tethys, which is in line with the tectonic and palaeogeographical position of the Mecsek Zone during the Late Jurassic. The ammonite assemblage represents elements of five Tethysian ammonite zones of the Kimmeridgian and Tithonian. The lower Kimmeridgian Herbichi Zone is indicated by Streblites tenuilobatus and Praesimoceras herbichi. The upper Kimmeridgian Acanthicum Zone is indicated by Aspidoceras acanthicum, and the Cavouri Zone by Mesosimoceras cavouri and Aspidoceras caletanum. The upper Kimmeridgian Beckeri Zone is suggested by Hybonoticeras pressulum and Pseudowaagenia inerme. Whereas Gravesia aff. gigas, Lithacoceras aff. siliceum, and Malagasites? denseplicatus are faunal elements characterising the Early Tithonian Hybonotum Zone. Phylloceratid and lytoceratid specimens account only for 12% of the fauna, while the majority of the specimens belong to the Oppeliidae and Ataxioceratidae (60%).}, year = {2021}, eissn = {1634-0744}, pages = {265-314}, orcid-numbers = {Bujtor, László/0000-0001-9699-7711} } @article{MTMT:32051184, title = {First record of late Valanginian ammonites from the Mecsek Mountains (Hungary), and their importance for regional stratigraphy}, url = {https://m2.mtmt.hu/api/publication/32051184}, author = {Bujtor, László and Gőgös, Gergő}, doi = {10.1007/s12542-021-00559-6}, journal-iso = {PALAEONTOL Z}, journal = {PALAEONTOLOGISCHE ZEITSCHRIFT}, volume = {95}, unique-id = {32051184}, issn = {0031-0220}, abstract = {A fairly preserved ammonite of Early Cretaceous age from the Mecsek Mountains, southern Hungary is described. Tescheniceras subpachydicranum is the first record of late Valanginian ammonites from the Mecsek tectonic zone from a previously unknown locality indicating the uppermost Valanginian Criosarasinella furcillata Zone. This is the first ammonite-supported evidence for the presence of upper Valanginian strata in the Mecsek Mountains that stretches the time-span of the continuous basinal sedimentation from the beginning of the Berriasian till the Valanginian. The new finding raises the possibility for the presence of the Hauterivian strata too, which was never recognised by ammonites.}, year = {2021}, eissn = {1867-6812}, pages = {447-452}, orcid-numbers = {Bujtor, László/0000-0001-9699-7711} } @article{MTMT:32502815, title = {Latest Oxfordian – earliest Kimmeridgian ammonite dominated fauna and microfacies from the ammonitico rosso-type Fonyászó Limestone Formation at Zengővárkony (Mecsek Mountains, Hungary)}, url = {https://m2.mtmt.hu/api/publication/32502815}, author = {Bujtor, László and Albrecht, Richárd Gyula}, doi = {10.7306/VJ.19.3}, journal-iso = {VOL JURASSIC}, journal = {VOLUMINA JURASSICA}, volume = {19}, unique-id = {32502815}, issn = {1731-3708}, year = {2021}, eissn = {1896-7876}, pages = {61-94}, orcid-numbers = {Bujtor, László/0000-0001-9699-7711} } @article{MTMT:31196493, title = {Lower Tithonian and lower Berriasian brachiopods from the Márévár Limestone Formation, Zengővárkony (Mecsek Mountains Hungary), and remarks on their palaeoenvironment}, url = {https://m2.mtmt.hu/api/publication/31196493}, author = {Bujtor, László and Albrecht, Richárd Gyula and Maróti, Dávid and Miklósy, Ákos}, doi = {10.1007/s12542-020-00513-y}, journal-iso = {PALAEONTOL Z}, journal = {PALAEONTOLOGISCHE ZEITSCHRIFT}, volume = {95}, unique-id = {31196493}, issn = {0031-0220}, abstract = {A new collection provided some brachiopods assigned to Lacunosella hoheneggeri, Pygope diphya and P. janitor from the lower Tithonian (Micracanthoceras ponti Zone) and lower Berriasian (Calpionella Zone), and from the limestone succession at Zengővárkony, Mecsek Mountains, Hungary. This is the first taxonomic description and photographic documentation of these fossils. We provide reliable documentation of pygopid brachiopods from the Mecsek Mountains, known since 1880, but previously not described. For the moment, three pygopid brachiopod species are reliably reported from the Mecsek Mountains: Pygope diphya, P. janitor and Pygites diphyioides. The Lacunosella hoheneggeri described herein is the first record of Berriasian rhynchonellide brachiopods from the Mecsek Mountains. The lower Berriasian brachiopods may belong to a normal palaeoenvironment, with the usual size distribution.}, year = {2021}, eissn = {1867-6812}, pages = {85-95}, orcid-numbers = {Bujtor, László/0000-0001-9699-7711} } @article{MTMT:32082518, title = {Oxfordian brachiopods from the ammonitico rosso-type Fonyászó Limestone formation at Zengővárkony, Mecsek Mountains, Hungary and their palaeoecological, palaeobiogeographical and palaeopathological significance}, url = {https://m2.mtmt.hu/api/publication/32082518}, author = {Bujtor, László and Albrecht, Richárd Gyula}, doi = {10.1007/s12542-021-00560-z}, journal-iso = {PALAEONTOL Z}, journal = {PALAEONTOLOGISCHE ZEITSCHRIFT}, volume = {96}, unique-id = {32082518}, issn = {0031-0220}, abstract = {Recent discovery of a previously unknown outcrop in the vicinity of the Zengővárkony lime-kilns (Mecsek Mountains, Hungary) provided a few identifiable Upper Oxfordian brachiopods that exhibit a truly Mediterranean (Tethyan) character. Dating of the outcrop is based on a rich ammonite fauna: Benetticeras benettii; Trimarginites ex gr. trimarginatus; Orthosphinctes (Orthosphinctes) ex gr. tiziani clearly indicate the Late Oxfordian. The brachiopod fauna indicates a deep-water marine environment and well oxygenated sea floor. Nucleata bouei and Pygope catulloi are recorded for the first time from the Mecsek Mountains. A pathologic specimen of Pygope catulloi is also recognized. Its ventral valve was injured in an early developmental stage that caused deformation of the left side, which was overgrown by the healthy right side and created an asymmetric adult shell shape. Cause of the injury is unclear but it provides further evidence for subsequent healing of brachiopods after being injured. This is the first description and illustration of Oxfordian brachiopods from the Mecsek Mountains, Hungary. The occurrence of Tethyan originating pygopid brachiopods in the Oxfordian strengthens earlier observations that from the Bathonian/Callovian Tethyan influence became overwhelming in the Mecsek Mountains fauna. Pygope catulloi strengthens records from Algeria that pygopid brachiopods may have occurred very early on the periphery of the Western Tethys.}, year = {2021}, eissn = {1867-6812}, pages = {51-65}, orcid-numbers = {Bujtor, László/0000-0001-9699-7711; Albrecht, Richárd Gyula/0000-0002-4337-0410} } @article{MTMT:32172098, title = {Anisotropic grossular-andradite garnets: Evidence of two stage skarn evolution from Rudnik, Central Serbia}, url = {https://m2.mtmt.hu/api/publication/32172098}, author = {Kostic, B and Sreckovic-Batocanin, D and Filipov, P and Tancic, P and Sokol, K}, doi = {10.31577/GeolCarp.72.1.2}, journal-iso = {GEOL CARPATH}, journal = {GEOLOGICA CARPATHICA}, volume = {72}, unique-id = {32172098}, issn = {1335-0552}, abstract = {This paper presents LA-ICP-MS data for garnets from the Rudnik skarn deposit (Serbia), which range from Grs(45-58)Adr(40-52)Alm(2-3 )in the core and Adr(70-97)Grs(2-29)Sps(1) in the rim displaying anisotropy and zoning. In spite of wide compositional variations the garnets near the end-member of andradite (Adr>90) are generally isotropic. Fe-rich rims exhibit LREE depletion and flat HREE pattern with weak negative Eu anomaly, including higher As and W contents. On the other side, the Fe-poorer core shows flat REE pattern without any significant enrichment or depletion of REE. except higher amounts of trace elements, such as U, Th and Zr. Presence of sulphide minerals indicates reduction conditions and Eu divalent state. Different REE behaviour is conditioned by Eu2+ in reduction conditions. The observed variations in optical features and garnet chemistry are the results of their two-stage evolution. The first stage and period of garnet growth is probably buffered by mineral dissolution and reactions in the country rock. The second stage is related to hydrothermal activity when W and Fe were brought into the system probably by a boiling process in the volcanic event in the late Oligocene 23.9 Ma.}, keywords = {MASS-SPECTROMETRY; FLUID; CU; LA-ICP-MS; DEPOSIT; TRACE-ELEMENT; GARNETS; skarn; RARE-EARTH-ELEMENTS; Grandite garnet; grandite; ZONED GRANDITE}, year = {2021}, eissn = {1336-8052}, pages = {17-25}, orcid-numbers = {Kostic, B/0000-0002-8746-8516; Tancic, P/0000-0002-4024-710X} } @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:32064406, title = {Torn Between Two Plates: Exhumation of the Cer Massif (Internal Dinarides) as a Far‐Field Effect of Carpathian Slab Rollback Inferred From 40 Ar/ 39 Ar Dating and Cross Section Balancing}, url = {https://m2.mtmt.hu/api/publication/32064406}, author = {Löwe, Georg and Schneider, Susanne and Sperner, Blanka and Balling, Philipp and Pfänder, Jörg A. and Ustaszewski, Kamil}, doi = {10.1029/2021TC006699}, journal-iso = {TECTONICS}, journal = {TECTONICS}, volume = {40}, unique-id = {32064406}, issn = {0278-7407}, year = {2021}, eissn = {1944-9194}, pages = {1-29}, orcid-numbers = {Löwe, Georg/0000-0002-5380-2109; Schneider, Susanne/0000-0002-8392-7711; Balling, Philipp/0000-0002-8439-6369; Ustaszewski, Kamil/0000-0002-1642-5842} } @article{MTMT:32172097, title = {Upper Triassic-Lower Jurassic continental carbonates from the Apuseni Mountains, Romania: facies, lithology and paleoenvironments}, url = {https://m2.mtmt.hu/api/publication/32172097}, author = {Mircescu, CV and Tamas, T and Bucur, II. and Sasaran, E and Ungureanu, R and Mircescu, V and Mircescu, E and Oprisa, A}, doi = {10.1007/s10347-021-00622-3}, journal-iso = {FACIES}, journal = {FACIES}, volume = {67}, unique-id = {32172097}, issn = {0172-9179}, abstract = {We studied deposits belonging to the Bihor Unit from the Northern Apuseni Mountains (Romania). The described outcrops are located in the SW of Ses Mountain and the northeastern Padurea Craiului Massif. We determined the depositional environment and the mechanisms controlling the accumulation of Upper Triassic-Lower Jurassic continental deposits. The sedimentary formations contain carbonate breccia and calcretes embedded in continental clay deposits. Late Triassic-Early Jurassic depositional processes were influenced by the inherited paleobasement of the subaerially exposed Middle Triassic deposits. Numerous fragments of Anisian and Ladinian carbonate deposits are encased in weathered clay deposits accumulated on karstification surfaces developed at the top of Middle Triassic limestones. We integrated facies analysis and clay mineralogy to obtain an accurate interpretation of the continental processes acting at the Triassic-Jurassic boundary in the northern part of the Apuseni Mountains. The composition of the carbonate pebbles is described in terms of the carbonate facies, whereas the clay mineralogy was determined by applying X-ray powder diffraction. Thirteen facies associations are described consisting of carbonate, siliciclastic and ferilitic rock types. Such facies indicate sediment accumulation in a continental, mixed carbonate-siliciclastic depositional environment. A Late Triassic exposure event was followed by an Early Jurassic (Hettangian) transgression. Two major facies types are identified on the basis of their depositional environment. The first category includes subaerially exposed Triassic carbonates and ferilitic facies, while the second category consists of transgressive siliciclastic facies from the basal Lower Jurassic (Hettangian) sediments. The existing data suggest continental deposition in alternating, arid-humid warm climate conditions at the Triassic-Jurassic transition.}, keywords = {EVOLUTION; TRANSITION; BASIN; CLIMATE-CHANGE; Clay minerals; record; BOUNDARY; Margin; Calcrete; Geology; Calcretes; Subaerial exposure; Microcodium; Microcodium}, year = {2021}, eissn = {1612-4820} } @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:32572186, title = {Assessing the representative elementary volume of rock types by X-ray computed tomography (CT) – a simple approach to demonstrate the heterogeneity of the Boda Claystone Formation in Hungary}, url = {https://m2.mtmt.hu/api/publication/32572186}, author = {Abutaha, Saja and Geiger, János and Gulyás, Sándor and Fedor, Ferenc}, doi = {10.2478/logos-2021-0018}, journal-iso = {GEOLOGOS}, journal = {GEOLOGOS}, volume = {27}, unique-id = {32572186}, issn = {1426-8981}, year = {2021}, eissn = {2080-6574}, pages = {157-172}, orcid-numbers = {Abutaha, Saja/0000-0001-8439-5895; Geiger, János/0000-0001-9359-5266; Gulyás, Sándor/0000-0002-3384-2381} } @article{MTMT:31904372, title = {Sauropterygian remains from the Middle Triassic of Villány, Hungary—new information on the aquatic reptile fauna of Tisza Megaunit (Triassic southern Eurasian shelf region)}, url = {https://m2.mtmt.hu/api/publication/31904372}, author = {Segesdi, Martin and Ősi, Attila}, doi = {10.1007/s12549-020-00480-x}, journal-iso = {PALAEOBIODIV PALAEOENV}, journal = {PALAEOBIODIVERSITY AND PALAEOENVIRONMENTS}, volume = {101}, unique-id = {31904372}, issn = {1867-1594}, year = {2021}, eissn = {1867-1608}, pages = {985-1011}, orcid-numbers = {Segesdi, Martin/0000-0003-4942-1810; Ősi, Attila/0000-0003-2967-997X} } @article{MTMT:32500247, title = {On the Sava Suture Zone: Post-Neotethyan oblique subduction and the origin of the Late Cretaceous mini-magma pools}, url = {https://m2.mtmt.hu/api/publication/32500247}, author = {Spahić, Darko and Gaudenyi, Tivadar}, doi = {10.1016/j.cretres.2021.105062}, journal-iso = {CRETACEOUS RES}, journal = {CRETACEOUS RESEARCH}, volume = {131}, unique-id = {32500247}, issn = {0195-6671}, year = {2021}, eissn = {1095-998X}, orcid-numbers = {Spahić, Darko/0000-0002-5832-0782; Gaudenyi, Tivadar/0000-0002-1843-2384} } @article{MTMT:31312175, title = {Early Cretaceous brachiopods from a hydrothermally influenced environment of the Mecsek Mountains (Zengővárkony, southern Hungary) and their palaeobiogeographical relationships}, url = {https://m2.mtmt.hu/api/publication/31312175}, author = {Vörös, Attila and Bujtor, László}, doi = {10.1016/j.cretres.2020.104497}, journal-iso = {CRETACEOUS RES}, journal = {CRETACEOUS RESEARCH}, volume = {114}, unique-id = {31312175}, issn = {0195-6671}, abstract = {New material and the investigation of old collections provided some 150 specimens of Early Cretaceous brachiopods from the Mecsek Mountains, Hungary. Taxonomic evaluation resulted in the identification of some species previously unknown from Hungary and confirmed the presence of some previously described species, too. In this paper Fortunella cf. fortunae Calzada, 1985, Lacunosella hoheneggeri (Suess, 1858), Monticlarella remesi Nekvasilova, 1977, Moutonithyris moutoniana (d’Orbigny, 1847), Karadagella ? aff. bilimeki (Suess, 1858), Nucleata veronica Nekvasilova, 1980 are described. This fauna is rather endemic. All the specimens reveal a unique phenomenon: they exhibit 25‒70% larger average dimensions compared to populations of their closest relatives or type localities. The uniform size increase of these brachiopods may be linked to hydrothermal processes of the sea-floor. Lately, a discovery from the Tyrrhenian Sea offers a Recent, present day analogue to this enigmatic palaeoenvironment. Palaeobiogeographic comparison of this small endemic fauna with eight others, mainly Hauterivian and Tethyan brachiopod assemblages reveals the distinct Sub-Tethyan domain consisting of the faunas from Zengővárkony, Codlea (Eastern Carpathians) and Štramberk (Czechia). This strengthens previously described affinities and relationships of these faunas and helps to clarify the Cretaceous palaeogeographic position of the Mecsek Mountains.}, year = {2020}, eissn = {1095-998X}, orcid-numbers = {Bujtor, László/0000-0001-9699-7711} } @article{MTMT:31386290, title = {Surface microtextures and new U–Pb dating of detrital zircons from the Eocene Strihovce sandstones in the Magura Nappe of the External Western Carpathians: implications for their provenance}, url = {https://m2.mtmt.hu/api/publication/31386290}, author = {Bónová, K and Pańczyk, M and Bóna, J}, doi = {10.1007/s00531-020-01859-z}, journal-iso = {INT J EARTH SCI}, journal = {INTERNATIONAL JOURNAL OF EARTH SCIENCES}, volume = {109}, unique-id = {31386290}, issn = {1437-3254}, year = {2020}, eissn = {1437-3262}, pages = {1565-1587} } @article{MTMT:30974514, title = {New kingenoid (Terebratellidina) brachiopods with larger body sizes from the Early Cretaceous of Zengővárkony (Mecsek Mountains, Hungary)}, url = {https://m2.mtmt.hu/api/publication/30974514}, author = {Bujtor, László and Vörös, Attila}, doi = {10.1017/jpa.2019.94}, journal-iso = {J PALEONTOL}, journal = {JOURNAL OF PALEONTOLOGY}, volume = {94}, unique-id = {30974514}, issn = {0022-3360}, year = {2020}, eissn = {1937-2337}, pages = {475-488}, orcid-numbers = {Bujtor, László/0000-0001-9699-7711} } @article{MTMT:31253429, title = {Paleofluid Fingerprint as an Independent Paleogeographic Correlation Tool: An Example from Pennsylvanian Sandstones and Neighboring Crystalline Rocks (Tisia Composite Terrane, S Hungary)}, url = {https://m2.mtmt.hu/api/publication/31253429}, author = {Fintor, Krisztián and Raucsikné Varga, Andrea Beáta}, doi = {10.1155/2020/3568986}, journal-iso = {GEOFLUIDS}, journal = {GEOFLUIDS}, volume = {2020}, unique-id = {31253429}, issn = {1468-8115}, year = {2020}, eissn = {1468-8123}, orcid-numbers = {Fintor, Krisztián/0000-0003-4794-9419; Raucsikné Varga, Andrea Beáta/0000-0002-8673-1482} } @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: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:31269081, title = {Az ImaGeo-magszkennelés módszerei egy mecseki fúrás nagy felbontású értelmezésének példáján.}, url = {https://m2.mtmt.hu/api/publication/31269081}, author = {Maros, Gyula and Sallay, Enikő and Ádámné Incze, Sz. and Hatvani, István Gábor and Palotás, Klára and Kovács, József and Gyenis, Á. and Gróf, Gyula István and Pásztor, Szilárd and Andrássy, L. and Mara, J. and Vihar, L. and Szongoth, G.}, doi = {10.23928/foldt.kozl.2020.150.1.81}, journal-iso = {FÖLDTANI KÖZLÖNY}, journal = {FÖLDTANI KÖZLÖNY}, volume = {150}, unique-id = {31269081}, issn = {0015-542X}, abstract = {A saját fejlesztésű ImaGeo-rendszer terepen, fúrásokban és bányatérségekben is nagy felbontású, digitális földtanidokumentációt és 3D földtani–tektonikai adatfelvételt tesz lehetővé, normál és UV-fény megvilágításban egyaránt. A fú rá -sokban kapott adatok mélyfúrás-geofizikai akusztikus (Borehole televiewer, BHTV) vagy ellenállás (pl. Formation Mic -roImager, FMI) adatsorok felhasználásával újra orientálhatóak és ezzel részletes földtani elemzések megvalósítása vá liklehetővé a valós térben. A rendszer részei a Magszkenner, a Fotórobot és a LIPS (Lézergerjesztésű plazmaspektrométer).Jelen cikk az ImaGeo-rendszer módszereinek bemutatása mellett esettanulmányt közöl az Ibafa, Ib–4 fúrás mezo -zoos rétegsorának magszkenneléses eredményeiről különös tekintettel a Jakabhegyi Homokkő Formáció elem zésére. AFor má ció vizsgálatát az adatok 45/13°-os (dőlésirány/dőlésszög) tektonikusan kibillentett helyzetből történt vissza -billentés után valósítottuk meg. A magszkennelésből származó szemcseméret-, rétegvastagság-, dőlésirány- és dőlés -szögeloszlások vizsgálata alapján a Jakabhegyi Homokkő Formáció harántolt rétegsorát 5 szakaszra lehetett bon tani. Aszakaszhatárok nem korrelálnak a földtani dokumentáció szakaszainak határaival. A visszabillentett dőlések DDK, D ésDNy felé mu tat nak, de bizonyos mélységszakaszokban a tisztán Ny-i és K-i irányok is jelentősek. Mindezeket üledék -szállítási fői rány ként értelmezzük. A szállítási irányok a formáció egészét tekintve is széles spektrumon oszlanak el. Arétegvastagság, dőlésirány- és dőlésszögadatok ciklicitáselemzését vizuálisan, mintázatok felismerése útján és geomate -matikai perio dicitáselemzéssel vizsgáltuk. Ezek alapján több, különböző periódushosszúságú (deciméteres, 1,3 és 8 mé -te res) ciklust lehetett meghatározni. A ciklusosság megállapítható a lemezvastagságban, a dőlésszögek és a dőlésirányok eloszlásában is. A hosszabb ciklusok leginkább a dőlésirányok eloszlásában mutatkoznak. A dőlésszögekben a vizuális,mintázatokon alapuló és a geomatematikai módszer is a 0,5 m körüli ciklust mutatta ki. A geomatematikai elemzés 2párhuzamos ciklus hosszt mutatott ki a dőlésirányokban és a dőlésszögekben. Ezek 1,3 és ~4,5 m ciklushosszúságú perió -dusok. A vizu ális elemzés feltárt egy mintegy 50 m-es ciklust is, ezt geomatematikai úton nem lehetett igazolni.}, year = {2020}, eissn = {2559-902X}, pages = {81-102}, orcid-numbers = {Maros, Gyula/0000-0002-2973-4513; Hatvani, István Gábor/0000-0002-9262-7315; Kovács, József/0000-0002-6797-2504; Gróf, Gyula István/0000-0002-6359-768X} } @article{MTMT:31614407, title = {Lithologically controlled behaviour of the Dorozsma metamorphic hydrocarbon reservoir (Pannonian Basin, SE Hungary)}, url = {https://m2.mtmt.hu/api/publication/31614407}, author = {M. Tóth, Tivadar and Vargáné Tóth, I}, doi = {10.1016/j.petrol.2020.107748}, journal-iso = {J PETROL SCI ENG}, journal = {JOURNAL OF PETROLEUM SCIENCE AND ENGINEERING}, volume = {195}, unique-id = {31614407}, issn = {0920-4105}, year = {2020}, eissn = {1873-4715}, orcid-numbers = {M. Tóth, Tivadar/0000-0003-1012-1095} } @article{MTMT:31385739, title = {Tanystropheus and other archosauromorph reptile remains from the Middle and Late Triassic of Villány (Villány Hills, Hungary)}, url = {https://m2.mtmt.hu/api/publication/31385739}, author = {Ősi, Attila and Szabó, Márton and Botfalvai, Gábor}, doi = {10.31577/GeolCarp.71.3.5}, journal-iso = {GEOL CARPATH}, journal = {GEOLOGICA CARPATHICA}, volume = {71}, unique-id = {31385739}, issn = {1335-0552}, year = {2020}, eissn = {1336-8052}, pages = {264-273}, orcid-numbers = {Ősi, Attila/0000-0003-2967-997X; Botfalvai, Gábor/0000-0002-5479-9036} } @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:31422845, title = {The early Paleozoic cumulate gabbroic rocks from the southwest part of the Tisza Mega-Unit (Mt. Papuk, NE Croatia): evidence of a Gondwana suture zone}, url = {https://m2.mtmt.hu/api/publication/31422845}, author = {Slovenec, Damir and Belak, Mirko and Misur, Ivan and Segvic, Branimir and Schuster, Ralf}, doi = {10.1007/s00531-020-01896-8}, journal-iso = {INT J EARTH SCI}, journal = {INTERNATIONAL JOURNAL OF EARTH SCIENCES}, volume = {109}, unique-id = {31422845}, issn = {1437-3254}, abstract = {The Mt. Papuk heteroadcumulate pyroxene-amphibole gabbronorites, which outcrops at the southern margin of the Tisza Mega-Unit, is suggested to stem from the deep oceanic crust formed by the in situ crystallisation in a supposed magma chamber. Amphibole oikocrystals are found to define a poikilitic texture of analysed rocks. A common enclosure in amphibole is the cumulus orthopyroxene, and rarely, the clinopyroxene and/or plagioclase and spinel. The chemical composition of related minerals and their crystallisation sequence suggest the sub-solidus crystallisation of gabbronorite in an open system at high temperatures and medium pressures. Parental magmas originated from the moderately depleted mantle source, which was metasomatised prior to melting. Early mineral fractionation gave rise to the assemblage consisted of spinel, pyroxene, plagioclase and intercumulus amphibole. The rocks' bulk chemistry, mineral crystallisation sequence, pyroxene geochemistry and myriad of high Ca-plagioclase, which coexists with igneous Ca-amphibole are all in favour of the strong subduction influence typical for mafic intrusion formed above mantle wedge in the root of an island arc at depths of 10-21 km. Herein presented geochemical and isotopic data (Ar-40-Ar-39: 487.1 +/- 4.3 Ma and Sm-Nd: 505 Ma) go along with the existence of an intra-oceanic arc related to geodynamic events that took place in the Prototethyan oceanic realm s.l. during middle Cambrian to earliest Ordovician. These events were likely correlated with the subduction of the Quaidam(?) back-arc ocean, or alternatively, with the subduction and closure of Prototethyan branches located between microcontinental fragments of Asia. Initially, the closure of back-arc oceans led to crust fragmentation and, then, addition of non-metamorphosed mafites into the obducted sequence further from the active continental margins of Gondwana and Laurassia at the time of the formation of Pangea in the late Palaeozoic.}, keywords = {MT; Papuk; Early Paleozoic; Cumulate gabbronorite; Intra-oceanic island arc; Tisza Mega-Unit; Gondwana suture zone}, year = {2020}, eissn = {1437-3262}, pages = {2209-2233}, orcid-numbers = {Slovenec, Damir/0000-0003-3251-827X; Segvic, Branimir/0000-0002-3769-7249} } @article{MTMT:31346919, title = {Shear strain and volume change associated with sigmoidal vein arrays in the Boda Claystone}, url = {https://m2.mtmt.hu/api/publication/31346919}, author = {Tóth, Emese and Hrabovszki, Ervin and M. Tóth, Tivadar and Schubert, Félix}, doi = {10.1016/j.jsg.2020.104105}, journal-iso = {J STRUCT GEOL}, journal = {JOURNAL OF STRUCTURAL GEOLOGY}, volume = {138}, unique-id = {31346919}, issn = {0191-8141}, year = {2020}, eissn = {1873-1201}, orcid-numbers = {Hrabovszki, Ervin/0000-0001-7914-6042; M. Tóth, Tivadar/0000-0003-1012-1095; Schubert, Félix/0000-0001-8647-5354} } @article{MTMT:31124485, title = {Orogenic architecture of the Mediterranean region and kinematic reconstruction of its tectonic evolution since the Triassic}, url = {https://m2.mtmt.hu/api/publication/31124485}, author = {van Hinsbergen, DJJ. and Torsvik, TH. and Schmid, SM. and Maţenco, LC. and Maffione, M and Vissers, RLM. and Gürer, D and Spakman, W}, doi = {10.1016/j.gr.2019.07.009}, journal-iso = {GONDWANA RES}, journal = {GONDWANA RESEARCH}, volume = {81}, unique-id = {31124485}, issn = {1342-937X}, year = {2020}, eissn = {1878-0571}, pages = {79-229}, orcid-numbers = {van Hinsbergen, DJJ./0000-0003-3410-0344; Maffione, M/0000-0002-9930-7699} } @article{MTMT:30461681, title = {Sedimentological characteristics and paleoenvironmental implication of Triassic vertebrate localities in Villány (Villány Hills, Southern Hungary)}, url = {https://m2.mtmt.hu/api/publication/30461681}, author = {Botfalvai, Gábor and Győri, Orsolya and Pozsgai, Emília and Farkas, MI and Sági, Tamás and Szabó, Márton and Ősi, Attila}, doi = {10.2478/geoca-2019-0008}, journal-iso = {GEOL CARPATH}, journal = {GEOLOGICA CARPATHICA}, volume = {70}, unique-id = {30461681}, issn = {1335-0552}, year = {2019}, eissn = {1336-8052}, pages = {135-152}, orcid-numbers = {Botfalvai, Gábor/0000-0002-5479-9036; Győri, Orsolya/0000-0002-3646-9113; Sági, Tamás/0000-0003-4664-5472; Ősi, Attila/0000-0003-2967-997X} } @article{MTMT:32589011, title = {New results of boda claystone research: Genesis, mineralogy, geochemistry, petrophysics}, url = {https://m2.mtmt.hu/api/publication/32589011}, author = {Fedor, Ferenc and Máthé, Zoltán and Ács, Péter and Koroncz, Péter János}, doi = {10.1144/SP482.13}, journal-iso = {GEOL SOC SPEC PUBL}, journal = {GEOLOGICAL SOCIETY SPECIAL PUBLICATIONS}, volume = {482}, unique-id = {32589011}, issn = {0305-8719}, year = {2019}, eissn = {2041-4927}, pages = {75-92} } @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: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: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:30590552, title = {Post-Variscan metamorphism in the Apuseni and Rodna Mountains (Romania): evidence from Sm-Nd garnet and U-Th-Pb monazite dating}, url = {https://m2.mtmt.hu/api/publication/30590552}, author = {Reiser, Martin Kaspar and Sabau, Gavril and Negulescu, Elena and Schuster, Ralf and Tropper, Peter and Fuegenschuh, Bernhard}, doi = {10.1007/s00015-018-0322-7}, journal-iso = {SWISS J GEOSCI}, journal = {SWISS JOURNAL OF GEOSCIENCES}, volume = {112}, unique-id = {30590552}, issn = {1661-8726}, abstract = {The Tisza and Dacia mega-units constitute a central part of the Alps-Carpathians-Dinarides orogenic system. Polyphase medium-grade metamorphism observed in mineral assemblages from the crystalline basement is often correlated with Variscan and pre-Variscan events. However, a mid-Cretaceous Sm-Nd garnet age (103.6 +/- 1.8Ma) from the Apuseni Mountains is at odds with this interpretation. Electron-microprobe U-Th-Pb dating of monazite in samples from the Apuseni Mountains, the Rodna Mountains, as well as the Simleu Silvaniei, Ticu and Preluca inselbergs revealed a complex pattern of Alpine and pre-Alpine age clusters. Pre-Variscan and Variscan ages were obtained from the core of zoned monazite grains and from samples that apparently escaped Alpine overprinting. Relic monazite in the latter is often replaced by rhabdophane and/or surrounded by allanite coronas. Permian to Early Triassic monazite ages correlate with the intrusion of granitic melts and pegmatites. Early Cretaceous ages from rims of chemically zoned grains and from monazite inclusions in garnet, biotite and staurolite represent newly formed metamorphic grains that crystallized on the prograde path during Alpine metamorphism. Petrographic observations of prograde allanite breakdown reactions, Sm-Nd garnet analyses and thermobaric estimates (500-550 degrees C/5-8kbar) from parts of the Tisza and Dacia mega-units constrain medium-grade conditions during Early Cretaceous times. Exclusively mid-Cretaceous monazite ages from the inselbergs and the Rebra-Unit of the Rodna Mountains, allow extending the Alpine prograde overprint across the Transylvanian basin. Together with other studies from the basement of the Pannonian basin, this implies that the Dacia Mega-Unit and parts of the Tisza Mega-Unit experienced a medium-grade metamorphic overprint and synkinematic garnet-growth during late Early Cretaceous times. The Alpine prograde medium-grade overprint is pronounced in the contact zone between the Tisza and Dacia mega-units and forms a continuous belt with the Cretaceous metamorphic imprint in the Eastern Alps, when back-rotated to its original position during the Cretaceous.}, keywords = {Cretaceous; TISZA; Medium-grade metamorphism; Dacia; Transylvania}, year = {2019}, eissn = {1661-8734}, pages = {101-120} } @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:30938641, title = {Taxonomical and palaeoecological investigations of the chondrichthyan and osteichthyan fish remains from the Middle-Late Triassic deposits of the Villány Hills (Southern Hungary)}, url = {https://m2.mtmt.hu/api/publication/30938641}, author = {Szabó, Márton and Botfalvai, Gábor and Ősi, Attila}, doi = {10.1016/j.geobios.2019.10.006}, journal-iso = {GEOBIOS-LYON}, journal = {GEOBIOS}, volume = {57}, unique-id = {30938641}, issn = {0016-6995}, year = {2019}, eissn = {1777-5728}, pages = {111-126}, orcid-numbers = {Botfalvai, Gábor/0000-0002-5479-9036; Ősi, Attila/0000-0003-2967-997X} } @article{MTMT:30644307, title = {Cements, Waters, and Scales: An Integrated Study of the Szeged Geothermal Systems (SE Hungary) to Characterize Natural Environmental Conditions of the Thermal Aquifer}, url = {https://m2.mtmt.hu/api/publication/30644307}, author = {Raucsikné Varga, Andrea Beáta and Bozsó, Gábor and Garaguly, István and Raucsik, Béla and Bencsik, Attila and Kóbor, Balázs}, doi = {10.1155/2019/4863814}, journal-iso = {GEOFLUIDS}, journal = {GEOFLUIDS}, volume = {2019}, unique-id = {30644307}, issn = {1468-8115}, year = {2019}, eissn = {1468-8123}, orcid-numbers = {Raucsikné Varga, Andrea Beáta/0000-0002-8673-1482; Garaguly, István/0000-0002-2802-0738; Raucsik, Béla/0000-0002-1951-5974} } @article{MTMT:30663414, title = {EAST VARDAR OPHIOLITES REVISITED: A BRIEF SYNTHESIS OF GEOLOGY AND GEOCHEMICAL DATA}, url = {https://m2.mtmt.hu/api/publication/30663414}, author = {Boev, Blažo and Cvetković, Vladica and Prelević, Dejan and Šarić, Kristina and Boev, Ivan}, doi = {10.20903/csnmbs.masa.2018.39.1.119}, journal-iso = {CONTRIBUT: MACEDON ACAD SCI ARTS}, journal = {PRILOZI: MAKEDONSKA AKDEMIJA NA NAUKITE I UMETNOSTITE ODDELENIE ZA PRIRODNO-MATEMATICKI I BIOTEHNICKI NAUKI / CONTRIBUTIONS: MACEDONIAN ACADEMY OF SCIENCES AND ARTS SECTION OF MATHEMATICAL AND TECHNICAL SCIENCES}, volume = {39}, unique-id = {30663414}, issn = {1857-9027}, year = {2018}, eissn = {1857-9949}, pages = {51-68} } @article{MTMT:27312440, title = {Heavy minerals and exotic pebbles from the Eocene flysch deposits of the Magura Nappe (Outer Western Carpathians, eastern Slovakia): their composition and implications on the provenance}, url = {https://m2.mtmt.hu/api/publication/27312440}, author = {Bonova, Katarina and Bona, Jan and Kovacik, Martin and Mikus, Tomas}, doi = {10.3906/yer-1707-9}, journal-iso = {TURK J EARTH SCI}, journal = {TURKISH JOURNAL OF EARTH SCIENCES}, volume = {27}, unique-id = {27312440}, issn = {1300-0985}, year = {2018}, eissn = {1303-619X}, pages = {64-88} } @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: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: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:3359490, title = {Environmental response to the early Toarcian carbon cycle and climate perturbations in the northeastern part of the West-Tethys shelf}, url = {https://m2.mtmt.hu/api/publication/3359490}, author = {Ruebsam, Wolfgang and Müller, Tamás and Kovács, János and Pálfy, József and Schwark, Lorenz}, doi = {10.1016/j.gr.2018.03.013}, journal-iso = {GONDWANA RES}, journal = {GONDWANA RESEARCH}, volume = {59}, unique-id = {3359490}, issn = {1342-937X}, abstract = {Early Toarcian (Early Jurassic; -183 Ma) climate and carbon cycle perturbations were accompanied by widespread accumulation of bituminous sediments, formed during the Toarcian Oceanic Anoxic Event (T-OAE). On the northwestern Tethyan shelf, organic carbon accumulation was particularly widespread in hydrodynamically restricted regions of the European Epicontinental Basin System (EEBS) where it peaked during the formation of euxinic waters extending into the photic zone. In the adjacent northeastern West Tethys shelf (NE-WTS), an area proximal to the deeper and better ventilated NW Tethys, deposition of strata enriched in organic matter was restricted to depressions of limited spatial extent. While numerous works have addressed the bituminous strata from the EEBS, evolution of environmental conditions and drivers of organic matter accumulation in areas proximal to the open Tethys have received much less attention.}, keywords = {HIGH-RESOLUTION; Biological Markers; SALINITY; ORGANIC-MATTER; Sea-level; weathering; Oceanic anoxic event; Mecsek Mountains; ISOTOPE EVIDENCE; Photic zone euxinia; Photic zone euxinia; Organic matter preservation; Sulfide loss; SW-GERMANY II; PHOTIC-ZONE ANOXIA; POSIDONIA BLACK SHALE}, year = {2018}, eissn = {1878-0571}, pages = {144-158}, orcid-numbers = {Kovács, János/0000-0001-7742-5515; Pálfy, József/0000-0001-9686-1849} } @article{MTMT:27570131, title = {Lower Jurassic Bahamian-type facies in the Choc Nappe (Tatra Mts, West Carpathians, Poland) influenced by paleocirculation in the Western Tethys}, url = {https://m2.mtmt.hu/api/publication/27570131}, author = {Rychlinski, T and Uchman, A and Gazdzicki, A}, doi = {10.1007/s10347-018-0528-1}, journal-iso = {FACIES}, journal = {FACIES}, volume = {64}, unique-id = {27570131}, issn = {0172-9179}, year = {2018}, eissn = {1612-4820} } @article{MTMT:3401535, title = {Heat flow modelling in the Transylvanian basin: Implications for the evolution of the intra-Carpathians area}, url = {https://m2.mtmt.hu/api/publication/3401535}, author = {Tiliță, M and Lenkey, László and Mațenco, L and Horváth, Ferenc and Surányi, Gergely and Cloetingh, S}, doi = {10.1016/j.gloplacha.2018.07.007}, journal-iso = {GLOBAL PLANET CHANGE}, journal = {GLOBAL AND PLANETARY CHANGE}, volume = {171}, unique-id = {3401535}, issn = {0921-8181}, abstract = {The evolution of sedimentary basins and their thermal structure are the result of the coupling between shallow crustal and deep lithospheric - mantle processes. When sources of shallow crustal deformation are not detectable, then deep lithospheric processes have the role to reveal the origin of these events. A particular method of investigating these deep processes is to evaluate their lithospheric thermal imprint, in particular when anomalous thermal values are exhibited. One such example is the Transylvanian Basin situated at the interior of the highly bended Carpathians chain, which shows lower heat flow values when compared with average cratonic values and even lower when compared with the neighbouring Pannonian extensional basin. The basin architecture suggests that a deep lithospheric - asthenospheric mechanism is responsible for Middle - Late Miocene subsidence, coeval with phases of Carpathian collision. The interplay between upper crustal evolution and deep lithospheric mechanics is investigated by means of 2D lithospheric-scaled heat flow modelling, simulating the present-day thermal regime of the basin. The heat flow correction for transient effects shows the great importance of paleoclimate and sedimentation during the evolution of the basin, calculated values being similar to 20% higher when compared with measured heat flow. The modelling implies that the low values of heat flow are the result of a combination of thermal effects of Middle - Upper Miocene sedimentation and the presence of depleted rocks in the basin basement, with their thickness dependent on the amount of enrichment in felsic magmatism during their evolution in a supra-subduction zone. The observations infer a thinned lower part of the mantle during the Miocene evolution of the basin, but the lithosphere thermal time constant suggests such changes do not affect the thermal regime at present day. Larger effects in the SE part of the basin are likely driven by the recent asthenospheric uplift due to the Vrancea slab descent.}, keywords = {Sequence stratigraphy; tectonic evolution; Transylvanian Basin; UPPER-MANTLE; Eastern Carpathians; thermal structure; thermal structure; Geography, Physical; 2D finite element thermal modelling; Dynamic topography; SOUTH APUSENI MOUNTAINS; SOUTHEASTERN CARPATHIANS; JURASSIC OPHIOLITES; SEISMIC-REFRACTION}, year = {2018}, eissn = {1872-6364}, pages = {148-166}, orcid-numbers = {Lenkey, László/0000-0003-4236-4075} } @article{MTMT:26752881, title = {Magmatic and tectonic history of Jurassic ophiolites and associated granitoids from the South Apuseni Mountains (Romania)}, url = {https://m2.mtmt.hu/api/publication/26752881}, author = {Gallhofer, D and von Quadt, A and Schmid, SM and Guillong, M and Peytcheva, I and Seghedi, I}, doi = {10.1007/s00015-016-0231-6}, journal-iso = {SWISS J GEOSCI}, journal = {SWISS JOURNAL OF GEOSCIENCES}, volume = {110}, unique-id = {26752881}, issn = {1661-8726}, year = {2017}, eissn = {1661-8734}, pages = {699-719}, orcid-numbers = {von Quadt, A/0000-0002-0539-7380} } @article{MTMT:3202162, title = {Középső-triász dolomitok képződésének története és töréses deformációja a Szegedi-medence területén}, url = {https://m2.mtmt.hu/api/publication/3202162}, author = {Garaguly, István and Raucsik, Béla and Raucsikné Varga, Andrea Beáta and Schubert, Félix}, doi = {10.23928/foldt.kozl.2017.147.1.39}, journal-iso = {FÖLDTANI KÖZLÖNY}, journal = {FÖLDTANI KÖZLÖNY}, volume = {147}, unique-id = {3202162}, issn = {0015-542X}, year = {2017}, eissn = {2559-902X}, pages = {39-60}, orcid-numbers = {Garaguly, István/0000-0002-2802-0738; Raucsik, Béla/0000-0002-1951-5974; Raucsikné Varga, Andrea Beáta/0000-0002-8673-1482; Schubert, Félix/0000-0001-8647-5354} } @article{MTMT:3125321, title = {New multiproxy record of the Jenkyns Event (also known as the Toarcian Oceanic Anoxic Event) from the Mecsek Mountains (Hungary): Differences, duration and drivers}, url = {https://m2.mtmt.hu/api/publication/3125321}, author = {Müller, Tamás and Price, GD and Bajnai, Dávid and Nyerges, Anita and Kesjár, D and Raucsik, Béla and Raucsikné Varga, Andrea Beáta and Judik, Katalin and Fekete, József and May, Zoltán and Pálfy, József}, doi = {10.1111/sed.12332}, journal-iso = {SEDIMENTOLOGY}, journal = {SEDIMENTOLOGY}, volume = {64}, unique-id = {3125321}, issn = {0037-0746}, keywords = {Carbon Isotopes; Fourier transform infrared spectroscopy; Toarcian; Oceanic anoxic event; Early Jurassic; nannoplankton biostratigraphy; elemental geochemistry; cyclostratigraphy}, year = {2017}, eissn = {1365-3091}, pages = {66-86}, orcid-numbers = {Bajnai, Dávid/0000-0002-4053-5056; Raucsik, Béla/0000-0002-1951-5974; Raucsikné Varga, Andrea Beáta/0000-0002-8673-1482; Pálfy, József/0000-0001-9686-1849} } @article{MTMT:3132886, title = {Provenance of the Upper Triassic siliciclastics of the Mecsek Mountains and Villány Hills (Pannonian Basin, Hungary). constraints to the Early Mesozoic paleogeography of the Tisza Megaunit}, url = {https://m2.mtmt.hu/api/publication/3132886}, author = {Pozsgai, Emília and Józsa, Sándor and Dunkl, István and Sebe, Krisztina and Thamóné Bozsó, Edit and Sajó, István and Dezső, József and von Eynatten, H}, doi = {10.1007/s00531-016-1406-0}, journal-iso = {INT J EARTH SCI}, journal = {INTERNATIONAL JOURNAL OF EARTH SCIENCES}, volume = {106}, unique-id = {3132886}, issn = {1437-3254}, abstract = {The Tisza Megaunit in the Southern Pannonian Basin formed part of the southern margin of the European Plate in the Early Mesozoic era. Its exact paleo-position and relation to other structural blocks is disputed for a long time. Detrital zircon U–Pb dating, heavy mineral analysis and petrographical examination of Carnian to Pliensbachian sandstone members lead to better understanding of the provenance of clastic deposits after the Ladinian–Carnian carbonate to siliciclastic facies shift in the Southwestern Tisza Megaunit. Investigations allow for constraining its paleogeographic relation to adjacent units. The Carnian and Pliensbachian siliciclastics of the Villány Hills derive from inside the Southwestern Tisza Megaunit, i.e. the medium-grade polymetamorphic rocks of the adjacent Slavonian Mountains or similar basement fragments. The Upper Triassic clastic deposits of the Mecsek Mountains most likely derive from Variscan felsic plutonic rocks of the local basement or partially from the Southern/Southwestern Bohemian Massif. About 200 Ma zircon U–Pb ages are tentatively interpreted as traces of synsedimentary distal volcanism in the Central Atlantic Magmatic Province.}, keywords = {EVOLUTION; PROVENANCE; sandstones; BOHEMIAN MASSIF; U-PB; HEAVY MINERAL ANALYSIS; Tisza Megaunit; Upper Triassic; VARISCAN OROGEN; SOUTHERN HUNGARY; CHRONOLOGICAL CONSTRAINTS; HEAVY MINERAL ASSEMBLAGES; MEDITERRANEAN ALPINE CHAINS; Detrital zircon U-Pb geochronology; Zircon ages}, year = {2017}, eissn = {1437-3262}, pages = {2005-2024}, orcid-numbers = {Józsa, Sándor/0000-0001-8219-0044; Sebe, Krisztina/0000-0002-4647-2199; Sajó, István/0000-0002-1228-1407} } @article{MTMT:26747238, title = {Constraints on the depositional age and tectonometamorphic evolution of marbles from the Biharia Nappe System (Apuseni Mountains, Romania)}, url = {https://m2.mtmt.hu/api/publication/26747238}, author = {Reiser, MK and Schuster, R and Tropper, P and Fuegenschuh, B}, doi = {10.1515/geoca-2017-0012}, journal-iso = {GEOL CARPATH}, journal = {GEOLOGICA CARPATHICA}, volume = {68}, unique-id = {26747238}, issn = {1335-0552}, year = {2017}, eissn = {1336-8052}, pages = {147-164} } @article{MTMT:26563610, title = {From nappe stacking to exhumation: Cretaceous tectonics in the Apuseni Mountains (Romania)}, url = {https://m2.mtmt.hu/api/publication/26563610}, author = {Reiser, MK and Schuster, R and Spikings, R and Tropper, P and Fuegenschuh, B}, doi = {10.1007/s00531-016-1335-y}, journal-iso = {INT J EARTH SCI}, journal = {INTERNATIONAL JOURNAL OF EARTH SCIENCES}, volume = {106}, unique-id = {26563610}, issn = {1437-3254}, year = {2017}, eissn = {1437-3262}, pages = {659-685} } @article{MTMT:3097539, title = {The link between tectonics and sedimentation in back-arc basins: New genetic constraints from the analysis of the Pannonian Basin}, url = {https://m2.mtmt.hu/api/publication/3097539}, author = {Balázs, Attila and Matenco, L and Magyar, Imre and Horváth, Ferenc and Cloetingh, S}, doi = {10.1002/2015TC004109}, journal-iso = {TECTONICS}, journal = {TECTONICS}, volume = {35}, unique-id = {3097539}, issn = {0278-7407}, abstract = {The architecture of sedimentary basins reflects the relationship between accommodation space and sediment supply, their rates and localization being variable during basin evolution. The mechanisms driving the interplay between tectonics and sedimentation in extensional back-arc basins overlying rheological weak zones inherited from an earlier orogenic evolution are less understood. A typical example is the Pannonian back-arc basin of Central Europe. It is floored by continental lithosphere and was affected by large amounts of extension driven by the subduction rollback that took place in the Carpathians and/or Dinarides. A novel kinematic and seismic sequence stratigraphic interpretation calibrated by wells allows the quantification of the link between the formation of half grabens and coeval sedimentation in the Great Hungarian Plain part of the basin. While the lower order tectonic-induced cycles characterize the main phases of extension in various subbasins, the higher-order cyclicity and associated unconformities define individual moments of fault (re)activation. Our novel interpretation of a temporal and spatial migration of extension during Miocene times explains the contrasting present-day strike of various subbasins as a result of their gradual clockwise rotation. Incorporating the observed asymmetry, in particular the associated footwall exhumation, infers that the amount of extension is much larger than previously thought. The quantitative link between tectonics and sedimentation has allowed the definition of a novel model of sedimentation in asymmetric basins that can be ported to other natural scenarios of similarly hyperextended back-arc basins observed elsewhere. ©2016. American Geophysical Union. All Rights Reserved.}, keywords = {STRATIGRAPHY; Pannonian Basin; carpathians; Tectonics; Structural geology; Lithology; Sedimentation; Inversion tectonics; Tectonic system; Back-arc extensions; tectonic system tracts; back-arc extension}, year = {2016}, eissn = {1944-9194}, pages = {1526-1559}, orcid-numbers = {Balázs, Attila/0000-0003-2948-0397} } @article{MTMT:3120888, title = {Multiphase response of palynomorphs to the Toarcian Oceanic Anoxic Event (Early Jurassic) in the Réka Valley section, Hungary}, url = {https://m2.mtmt.hu/api/publication/3120888}, author = {Baranyi, Viktória and Pálfy, József and Görög, Ágnes and Riding, James B and Raucsik, Béla}, doi = {10.1016/j.revpalbo.2016.09.011}, journal-iso = {REV PALAEOBOT PALYNO}, journal = {REVIEW OF PALAEOBOTANY AND PALYNOLOGY}, volume = {235}, unique-id = {3120888}, issn = {0034-6667}, abstract = {Abstract Major palaeoenvironmental and palaeoceanographical changes occurred during the Early Jurassic Toarcian Oceanic Anoxic Event (T-OAE), due to a perturbation of the global carbon cycle and a crisis in marine ecosystems. The sequence of environmental change and regional differences during the T-OAE are not yet fully understood and organic-walled phytoplankton and other palynomorphs are well-suited, but under-utilised, in research into this event. Based on quantitative palynological analyses from a black shale-bearing succession at Réka Valley in the Mecsek Mountains of southwest Hungary, five sequential palynomorph assemblages are distinguished. These reveal major shifts in organic-walled phytoplankton communities, driven by palaeoenvironmental changes. In addition, palynofacies analysis helped to document changes in the composition of sedimentary organic matter, and to quantify the terrestrial input. Assemblage 1 is characterised by a moderately diverse phytoplankton community and high levels of terrestrial palynomorphs. Assemblage 2 records a significant peak of the euryhaline dinoflagellate cyst Nannoceratopsis. Assemblage 3 is distinguished by dominance of highly opportunistic prasinophytes and the temporary disappearance of all dinoflagellate cyst taxa. Assemblages 4 and 5 represent distinctive phases of a prolonged recovery phase with low diversity phytoplankton assemblages and intermittently high levels of terrestrially-derived palynomorphs. The successive disappearance of phytoplankton taxa and the gradual takeover by opportunistic euryhaline species at the onset of the T-OAE were related to several phenomena. These include reduced salinity in the surface waters, establishment of a stable pycnocline and deterioration of nutrient recycling, followed by oxygen deficiency throughout much of the water column. The high amount of terrestrially-derived palynodebris indicates intense runoff and freshwater input, driven by the early Toarcian warming and the enhanced hydrological cycle. Comparison with coeval European successions proves that the palaeoenvironmental changes during the T-OAE were not entirely synchronous, and local factors played a crucial role in influencing phytoplankton communities. In the Mecsek Basin, regional freshening of the surface waters and increased terrestrial input due to the proximity of the hinterland had a greater influence on phytoplankton communities compared to the open oceanic setting of the Tethys to the south.}, keywords = {Hungary; Palynofacies; Mecsek Mountains; DINOFLAGELLATE CYSTS; Early Jurassic; Toarcian Oceanic Anoxic Event (T-OAE); prasinophytes}, year = {2016}, eissn = {1879-0615}, pages = {51-70}, orcid-numbers = {Baranyi, Viktória/0000-0002-1194-9903; Pálfy, József/0000-0001-9686-1849; Görög, Ágnes/0000-0002-0910-8822; Raucsik, Béla/0000-0002-1951-5974} } @article{MTMT:32915453, title = {Geology of south-eastern Europe}, url = {https://m2.mtmt.hu/api/publication/32915453}, author = {Cvetkovic, V. and Prelević, D. and Schmid, S.}, doi = {10.1007/978-3-319-25379-4_1}, journal-iso = {ENVIRON EARTH SCI}, journal = {ENVIRONMENTAL EARTH SCIENCES}, volume = {2016}, unique-id = {32915453}, issn = {1866-6280}, abstract = {The region of South-Eastern Europe (SEE) occupies an important segment of the Alpine-Himalayan collisional orogenic belt and consists of several Phanerozoic mobile belts. The SEE region inherits its geology from the evolution of the Vardar Tethys ocean, which existed in-between the Eurasian (Europe) and Gondwana (Africa) continental plates and which relicts presently occur along the Vardar-Tethyan mega-suture. This synthesis, therefore, consists of (1) pre-, (2) syn- and (3) post-Vardar-Tethyan geology of SEE. Pre-Vardar-Tethyan geology on the European side is reflected by geological units formed from Precambrian to Mesozoic times and include the Moesian platform, the Dacia mega-unit and the Rhodopes. On the Gondwana side, it is represented by the External Dinarides, the Dalmatian-Ionian Zone and Stable Adria (Apulia), all principally formed from Paleozoic to Mesozoic times. The Syn-Vardar-Tethyan units encompass the bulk of the geological framework of SEE. They are a physical record of the former existence of the Mesozoic oceanic lithosphere, being represented dominantly by ophiolites and trench/accretionary wedge (melange) assemblages, which originated and were reworked during the life-span of the Vardar Tethys. The Post-Vardar-Tethyan geological evolution refers to the time period from the final closure of the Vardar Tethys until present. It comprises all rocks that stratigraphically overlie the Vardar-Tethyan mega-suture and seal the contacts between the mega-suture and the surrounding geological units. This is the time characterized by rapid extension coupled with exhumation of the lower crustal material, high heat flow, both intrusive and extrusive magmatism and considerable lithosphere thinning.}, year = {2016}, eissn = {1866-6299}, pages = {1-29} } @article{MTMT:25601726, title = {First sauropod bones from Italy offer new insights on the radiation of Titanosauria between Africa and Europe}, url = {https://m2.mtmt.hu/api/publication/25601726}, author = {Dal Sasso, C and Pierangelini, G and Famiani, F and Cau, A and Nicosia, U}, doi = {10.1016/j.cretres.2016.03.008}, journal-iso = {CRETACEOUS RES}, journal = {CRETACEOUS RESEARCH}, volume = {64}, unique-id = {25601726}, issn = {0195-6671}, year = {2016}, eissn = {1095-998X}, pages = {88-109} } @article{MTMT:3167421, title = {Re-evaluation of archive pebble distribution data for the Upper Permian Bakonya Sandstone Member of the Kővágószőlős Formation, Hungary — a comparison with the composition of cores BAF–1 and BAF–1A}, url = {https://m2.mtmt.hu/api/publication/3167421}, author = {Magyar, Levente and Benei, Balázs and Halász, Amadé}, journal-iso = {FÖLDTANI KÖZLÖNY}, journal = {FÖLDTANI KÖZLÖNY}, volume = {146}, unique-id = {3167421}, issn = {0015-542X}, year = {2016}, eissn = {2559-902X}, pages = {223-232}, orcid-numbers = {Halász, Amadé/0000-0003-4582-8883} } @article{MTMT:3071286, title = {Clay mineralogy of the Boda Claystone Formation (Mecsek Mts., SW Hungary)}, url = {https://m2.mtmt.hu/api/publication/3071286}, author = {Németh, Tibor and Máthé, Z and Pekker, Péter and Dódony, István and Kovácsné Kis, Viktória and Sipos, Péter and Cora, Ildikó and Kovács, Ivett}, doi = {10.1515/geo-2016-0024}, journal-iso = {OPEN GEOSCI}, journal = {OPEN GEOSCIENCES}, volume = {8}, unique-id = {3071286}, issn = {2391-5447}, abstract = {Boda Claystone Formation (BCF) is the host rock of the planned site for high level nuclear waste repository inHungary. Samples representing the dominant rock types of BCF were studied: albitic claystone, claystone with high illite content, and analcime bearing claystone. Clay minerals in these three rock types were characterized by Xray powder diffraction (XRD), transmission electron microscopy (TEM) and thermal analysis (DTA-TG), and the results were discussed from the point of view of the radionuclide sorption properties being studied in the future. Mineral compositions of bulk BCF samples vary in wide ranges. In the albitic sample, besides the dominant illite, few percent of chlorite represents the layer silicates in the clay fraction. Illite is the dominating phase in the illitic sample, with a few percent of chlorite. HRTEM study revealed that the thickness of illite particles rarely reaches 10 layers, usually are of 5-6 TOT layer thick. Illite crystals are generally thicker in the albitic sample than in the illitic one. The significant difference between the clay mineral characterisitics of the analcimous and the other two samples is that the former contains regularly interstratified chlorite/smectite beside the dominant illite. Based on the structural and chemical data two illite type minerals are present in the BCF samples: 1M polytype containing octahedral Fe and Mg besides Al, 2M polytype illite generally is free of Fe andMg. Close association of very thin illite plates and nanosized hematite crystals is typical textural feature for BCF. The goal of this study is to provide solid mineralogical basis for further studies focusing on radionuclide sorption properties. © 2016 T. Németh et al., published by De Gruyter Open.}, keywords = {HRTEM; analcime; Hematite; Nuclear waste repository; illite polytypes}, year = {2016}, eissn = {2391-5447}, pages = {259-274}, orcid-numbers = {Németh, Tibor/0000-0002-1836-6006; Pekker, Péter/0000-0002-0463-0742; Sipos, Péter/0000-0002-8746-0573; Kovács, Ivett/0000-0001-7015-7909} } @article{MTMT:2949640, title = {Localisation of ductile and brittle shear zones along the Szentlőrinc-1 well in the Mecsekalja Zone using quartz microstructural and well-log data}, url = {https://m2.mtmt.hu/api/publication/2949640}, author = {Skultéti, Ágnes and M. Tóth, Tivadar}, doi = {10.1007/s40328-015-0127-3}, journal-iso = {ACTA GEOD GEOPHYS}, journal = {ACTA GEODAETICA ET GEOPHYSICA}, volume = {51}, unique-id = {2949640}, issn = {2213-5812}, year = {2016}, eissn = {2213-5820}, pages = {295-314}, orcid-numbers = {M. Tóth, Tivadar/0000-0003-1012-1095} } @article{MTMT:25378640, title = {A sequence stratigraphic model for the Upper Miocene-Pliocene basin fill of the Pannonian Basin, eastern Hungary}, url = {https://m2.mtmt.hu/api/publication/25378640}, author = {Csato, I and Toth, S and Catuneanu, O and Granjeon, D}, doi = {10.1016/j.marpetgeo.2015.02.010}, journal-iso = {MAR PETROL GEOL}, journal = {MARINE AND PETROLEUM GEOLOGY}, volume = {66}, unique-id = {25378640}, issn = {0264-8172}, year = {2015}, eissn = {1873-4073}, pages = {117-134} } @article{MTMT:25365826, title = {Tectonic, magmatic, and metallogenic evolution of the Late Cretaceous arc in the Carpathian-Balkan orogen}, url = {https://m2.mtmt.hu/api/publication/25365826}, author = {Gallhofer, Daniela and von Quadt, Albrecht and Peytcheva, Irena and Schmid, Stefan M and Heinrich, Christoph A}, doi = {10.1002/2015TC003834}, journal-iso = {TECTONICS}, journal = {TECTONICS}, volume = {34}, unique-id = {25365826}, issn = {0278-7407}, year = {2015}, eissn = {1944-9194}, pages = {1813-1836} } @article{MTMT:2989417, title = {The colour analysis method applied to homogeneous rocks}, url = {https://m2.mtmt.hu/api/publication/2989417}, author = {Halász, Amadé and Halmai, Ákos}, doi = {10.1515/logos-2015-0019}, journal-iso = {GEOLOGOS}, journal = {GEOLOGOS}, volume = {21}, unique-id = {2989417}, issn = {1426-8981}, abstract = {Computer-aided colour analysis can facilitate cyclostratigraphic studies. Here we report on a case study involving the development of a digital colour analysis method for examination of the Boda Claystone Formation which is the most suitable in Hungary for the disposal of high-level radioactive waste. Rock type colours are reddish brown or brownish red, or any shade between brown and red. The method presented here could be used to differentiate similar colours and to identify gradual transitions between these; the latter are of great importance in a cyclostratigraphic analysis of the succession. Geophysical well-logging has demonstrated the existence of characteristic cyclic units, as detected by colour and natural gamma. Based on our research, colour, natural gamma and lithology correlate well. For core Ib-4, these features reveal the presence of orderly cycles with thicknesses of roughly 0.64 to 13 metres. Once the core has been scanned, this is a time- and cost-effective method.}, keywords = {ImageJ}, year = {2015}, eissn = {2080-6574}, pages = {233-239}, orcid-numbers = {Halász, Amadé/0000-0003-4582-8883; Halmai, Ákos/0000-0001-5722-8119} } @article{MTMT:2719067, title = {Evolution of the Pannonian basin and its geothermal resources}, url = {https://m2.mtmt.hu/api/publication/2719067}, author = {Horváth, Ferenc and Musitz, Balázs and Balázs, Attila and Végh, Andor and Uhrin, András and Nádor, Annamária and Koroknai, B and Pap, Norbert and Tóth, Tamás and Wórum, G}, doi = {10.1016/j.geothermics.2014.07.009}, journal-iso = {GEOTHERMICS}, journal = {GEOTHERMICS}, volume = {53}, unique-id = {2719067}, issn = {0375-6505}, keywords = {Pannonian Basin; Tectonics; Geothermal installations; Thermal water reservoirs}, year = {2015}, eissn = {1879-3576}, pages = {328-352}, orcid-numbers = {Balázs, Attila/0000-0003-2948-0397; Pap, Norbert/0000-0001-8243-4213} } @article{MTMT:25371198, title = {Assessing provenance of Upper Cretaceous siliciclastics using spectral gamma-ray record}, url = {https://m2.mtmt.hu/api/publication/25371198}, author = {Simicek, Daniel and Babek, Ondrej}, doi = {10.1515/geoca-2015-0028}, journal-iso = {GEOL CARPATH}, journal = {GEOLOGICA CARPATHICA}, volume = {66}, unique-id = {25371198}, issn = {1335-0552}, year = {2015}, eissn = {1336-8052}, pages = {311-329} } @article{MTMT:25373467, title = {Modelling the coupling between salt kinematics and subsidence evolution: Inferences for the Miocene evolution of the Transylvanian Basin}, url = {https://m2.mtmt.hu/api/publication/25373467}, author = {Tilita, M and Scheck-Wenderoth, M and Matenco, L and Cloetingh, S}, doi = {10.1016/j.tecto.2015.07.021}, journal-iso = {TECTONOPHYSICS}, journal = {TECTONOPHYSICS}, volume = {658}, unique-id = {25373467}, issn = {0040-1951}, year = {2015}, eissn = {1879-3266}, pages = {169-185} } @article{MTMT:2968441, title = {Loading and dilution: arsenic, sodium and nutrients in a section of the River Tisza, Hungary}, url = {https://m2.mtmt.hu/api/publication/2968441}, author = {Türk, Gábor and Prokisch, József and Simon, Edina and Szabó, Szilárd}, doi = {10.1515/geo-2015-0035}, journal-iso = {OPEN GEOSCI}, journal = {OPEN GEOSCIENCES}, volume = {7}, unique-id = {2968441}, issn = {2391-5447}, year = {2015}, eissn = {2391-5447}, pages = {627-636}, orcid-numbers = {Szabó, Szilárd/0000-0002-2670-7384} } @article{MTMT:25163708, title = {The tectonic evolution of a critical segment of the Dinarides-Alps connection: Kinematic and geochronological inferences from the Medvednica Mountains, NE Croatia}, url = {https://m2.mtmt.hu/api/publication/25163708}, author = {Van, Gelder IE and Matenco, L and Willingshofer, E and Tomljenovic, B and Andriessen, PAM and Ducea, MN and Beniest, A and Gruić, A}, doi = {10.1002/2015TC003937}, journal-iso = {TECTONICS}, journal = {TECTONICS}, volume = {34}, unique-id = {25163708}, issn = {0278-7407}, year = {2015}, eissn = {1944-9194}, pages = {1952-1978} } @article{MTMT:2964506, title = {Strike-slip tectonics in the Pannonian basin based on seismic surveys at Lake Balaton}, url = {https://m2.mtmt.hu/api/publication/2964506}, author = {Visnovitz, Ferenc and Horváth, Ferenc and Fekete, N and Spiess, V}, doi = {10.1007/s00531-015-1179-x}, journal-iso = {INT J EARTH SCI}, journal = {INTERNATIONAL JOURNAL OF EARTH SCIENCES}, volume = {104}, unique-id = {2964506}, issn = {1437-3254}, abstract = {Strike-slip tectonics has been the dominant style of deformation during the neotectonic (Pliocene and Quaternary) evolution of the Pannonian basin. Main faults are exposed in the “island mountains” of the basin, but strike-slip tectonic features can be best studied in the basin fill by seismic data. Lake Balaton offers the opportunity to carry out high to ultra-high-resolution seismo-acoustic surveys to image stratigraphic and tectonic features in the central part of the Pannonian basin. Several campaigns in the lake using different acquisition techniques have resulted in more than 2000-km seismo-acoustic profiles with a range of resolutions and penetration depths. Interpretation of faults and folds shows a few kilometers wide shear zone below the lake in Late Miocene–Pliocene strata. This zone can be identified as the continuation of the Balatonfő line known onshore to the east of the lake. Mapping revealed a set of duplex structures and highlighted the importance of this shear zone in the formation of Lake Balaton. Comparison of our results to analogue clay models suggests that the observed shear zone is sinistral and the horizontal displacement is on the order of hundreds of meters. Looking at 3D industrial seismic data to the south of the lake, we suggest that the first-order Balaton line, which represents the continuation of Periadriatic line, is also sinistral and characterized by small horizontal displacement of about 1.0–1.5 km during Pliocene and Quaternary times. This indicates a 0.2–0.3 mm/year average slip rate, which is compatible with recent GPS measurements.}, year = {2015}, eissn = {1437-3262}, pages = {2273-2285}, orcid-numbers = {Visnovitz, Ferenc/0000-0002-7040-0080} } @article{MTMT:2469969, title = {Allanite and monazite occurrences in variscan granitoids of Tisza Mega-Unit (South Hungary)}, url = {https://m2.mtmt.hu/api/publication/2469969}, author = {Buda, György and Nagy, G and Pál-Molnár, Elemér}, journal-iso = {CARPATH J EARTH ENVIRON SCI}, journal = {CARPATHIAN JOURNAL OF EARTH AND ENVIRONMENTAL SCIENCES}, volume = {9}, unique-id = {2469969}, issn = {1842-4090}, year = {2014}, eissn = {1844-489X}, pages = {57-68}, orcid-numbers = {Pál-Molnár, Elemér/0000-0002-9606-0133} } @article{MTMT:2474978, title = {Lithology identification using open-hole well-log data in the metamorphic Kiskunhalas-NE hydrocarbon reservoir, South Hungary}, url = {https://m2.mtmt.hu/api/publication/2474978}, author = {Fiser-Nagy, Ágnes and Varga-Tóth, I and M. Tóth, Tivadar}, doi = {10.1007/s40328-013-0037-1}, journal-iso = {ACTA GEOD GEOPHYS}, journal = {ACTA GEODAETICA ET GEOPHYSICA}, volume = {49}, unique-id = {2474978}, issn = {2213-5812}, abstract = {in press}, year = {2014}, eissn = {2213-5820}, pages = {57-78}, orcid-numbers = {M. Tóth, Tivadar/0000-0003-1012-1095} } @article{MTMT:23827609, title = {Provenance of Paleozoic very low- to low-grade metasedimentary rocks of South Tisia (Slavonian Mountains, Radlovac Complex, Croatia)}, url = {https://m2.mtmt.hu/api/publication/23827609}, author = {Bisevac, V and Krenn, E and Finger, F and Luzar-Oberiter, B and Balen, D}, doi = {10.2478/geoca-2013-0001}, journal-iso = {GEOL CARPATH}, journal = {GEOLOGICA CARPATHICA}, volume = {64}, unique-id = {23827609}, issn = {1335-0552}, year = {2013}, eissn = {1336-8052}, pages = {3-22} } @article{MTMT:2091219, title = {Valanginian perisphinctid ammonites from the Kisújbánya Basin (Eastern Mecsek Mts., Hungary)}, url = {https://m2.mtmt.hu/api/publication/2091219}, author = {Bujtor, László}, doi = {10.1016/j.cretres.2012.10.001}, journal-iso = {CRETACEOUS RES}, journal = {CRETACEOUS RESEARCH}, volume = {41}, unique-id = {2091219}, issn = {0195-6671}, abstract = {The most complete Hungarian Valanginian perisphinctid ammonite fauna of the Mecsek Mountains (South Hungary) consists of 14 species is reported. Thurmanniceras sp. aff. otopeta, Fuhriella michaelis, F. cf. hoheneggeri, Sarasinella cf. ambigua, Neocomites (Neocomites) subtenuis, Neocomites (Eristavites) platycostatus are reported for the first time from Hungary. The fauna comprises 23 ammonite species and is reported from Valanginian tuffaceous marl, alternating marl–limestone beds and loose limestone blocks. Two studied sections represent the Lower Valanginian Thurmanniceras pertransiens and partly the Busnardoites campylotoxus Zones while ammonites from loose blocks indicate the latter and possibly the Upper Valanginian Saynoceras verrucosum Zone. Variations in the faunal composition of the marl beds and the limestone blocks respectively, refer to the contrast between the ammonite ecological demands. Phylloceratid and lytoceratid ammonites prevail the marl beds, while olcostephanid and neocomitid ammonites prevail the shallower platform-like limestones. Sediment accumulation rate in that palaeo volcano related environment was high and bottom currents frequently washed together ammonite shells or filled their body chambers with smaller ammonite shell fragments. Due to the fast sedimentation the sections represent only partially the recognized ammonite zones therefore long-term or even infra-regional correlation was not possible. Palaeobiogeographically, the ammonite fauna has Mediterranean character and it shows close relationships to the Valanginian faunas of the Bakony Mts. (Hungary), Western Carpathians (Slovakia), Northern Calcareous Alps (Austria), and SE Spain. The presence of Fuhriella species is remarkable and enlarges our knowledge on the distribution of this enigmatic ammonite taxon adding new data to its Valanginian stratigraphic position and geographic distribution.}, year = {2013}, eissn = {1095-998X}, pages = {1-16}, orcid-numbers = {Bujtor, László/0000-0001-9699-7711} } @article{MTMT:2464910, title = {From continental platform towards rifting of the Tisza Unit in the Late Triassic to Early Cretaceous}, url = {https://m2.mtmt.hu/api/publication/2464910}, author = {Császár, Géza and Szinger, Balázs and Piros, Olga}, doi = {10.2478/geoca-2013-0020}, journal-iso = {GEOL CARPATH}, journal = {GEOLOGICA CARPATHICA}, volume = {64}, unique-id = {2464910}, issn = {1335-0552}, abstract = {The Upper Triassic-Lower Cretaceous successions of the Transdanubian part of the Mecsek and Villany-Bihor Zones of the Tisza Unit have been studied from the lithological, lithostratigraphical, sedimentological, microfossil and microfacies points of view in order to correlate and interpret the significant differences between them and to draw a conclusion about their geological and paleogeographical history. After an overview of the paleogeographical reconstructions of the broader area, the succession of the Mecsek and Villany-Bihor Zones and the debated Mariakemend-Bar Range are introduced. Until the end of the Middle Triassic the study area acted as an entity. The first fundamental difference between the two zones can be recognized in the Late Triassic when marine carbonates were replaced by thick fluvial siliciclastics in the Mecsek Zone, while it is represented only by small, local lenses with a few and thin dolostone intercalations in the Villany Zone. The Mecsek Zone is bordered southward by one of the large listric faults to the north of which very thick siliciclastics developed in the Early to Middle Jurassic, whereas it is highly lacunose in the larger western part of the Villany-Bihor Zone. The break at the base is subaerial, higher in the succession it is shallow submarine. The sediment is silty, occasionally sandy crinoidal limestone of late Early Jurassic or even Middle Jurassic in age. The Upper Jurassic in the Mecsek Zone is composed of deep-water cherty limestone while in the Villany Zone it became a thick, shallowing pelagic limestone with reworked patch reef fragments. It is clear evidence that the Mecsek Zone had a thinned continental crust thanks to the nearby rift zone while in the Villany Zone the crust remained thick. The actualized version of the Plasienka's paleogeographical model (Plasienka 2000) is introduced.}, keywords = {REGION; EVOLUTION; RECONSTRUCTION; Hungary; rifting; facies analysis; paleogeography; plate tectonics; MOUNTAINS; lithostratigraphy; Lower Cretaceous; Tisza unit; Upper Triassic}, year = {2013}, eissn = {1336-8052}, pages = {279-290} } @article{MTMT:2414426, title = {The origin and role of a calcite-filled microcrack generation in a metamorphic crystalline complex: The characterization of a fossilised seismic permeability system}, url = {https://m2.mtmt.hu/api/publication/2414426}, author = {Dabi, Gergely and Bajnóczi, Bernadett and Schubert, Félix and M. Tóth, Tivadar}, doi = {10.1016/j.tecto.2013.07.039}, journal-iso = {TECTONOPHYSICS}, journal = {TECTONOPHYSICS}, volume = {608}, unique-id = {2414426}, issn = {0040-1951}, year = {2013}, eissn = {1879-3266}, pages = {792-803}, orcid-numbers = {Bajnóczi, Bernadett/0000-0003-0006-7611; Schubert, Félix/0000-0001-8647-5354; M. Tóth, Tivadar/0000-0003-1012-1095} } @article{MTMT:23598142, title = {Thermal history of the Maramureş area (Northern Romania) constrained by zircon fission track analysis: Cretaceous metamorphism and Late Cretaceous to Paleocene exhumation}, url = {https://m2.mtmt.hu/api/publication/23598142}, author = {Gröger, HR and Tischler, M and Fügenschuh, B and Schmid, SM}, doi = {10.2478/geoca-2013-0026}, journal-iso = {GEOL CARPATH}, journal = {GEOLOGICA CARPATHICA}, volume = {64}, unique-id = {23598142}, issn = {1335-0552}, year = {2013}, eissn = {1336-8052}, pages = {383-398} } @article{MTMT:24076647, title = {Fission-track constraints on the thermal and tectonic evolution of the Apuseni Mountains (Romania)}, url = {https://m2.mtmt.hu/api/publication/24076647}, author = {Kounov, A and Schmid, SM}, doi = {10.1007/s00531-012-0800-5}, journal-iso = {INT J EARTH SCI}, journal = {INTERNATIONAL JOURNAL OF EARTH SCIENCES}, volume = {102}, unique-id = {24076647}, issn = {1437-3254}, year = {2013}, eissn = {1437-3262}, pages = {207-233} } @article{MTMT:2196221, title = {New paleomagnetic results from the Upper Cretaceous red marls of the Pieniny Klippen Belt, Western Carpathians: evidence for general CCW rotation and implications for the origin of the structural arc formation}, url = {https://m2.mtmt.hu/api/publication/2196221}, author = {Márton Péterné Szalay, Emőke and Grabowski, J and Plašienka, D and Túnyi, I and Krobicki, M and Haas, János and Pethe, Mihály}, doi = {10.1016/j.tecto.2013.01.027}, journal-iso = {TECTONOPHYSICS}, journal = {TECTONOPHYSICS}, volume = {592}, unique-id = {2196221}, issn = {0040-1951}, year = {2013}, eissn = {1879-3266}, pages = {1-13}, orcid-numbers = {Márton Péterné Szalay, Emőke/0000-0002-2135-8867; Haas, János/0000-0003-0929-8889} } @article{MTMT:2190426, title = {Integrated core study of a fractured metamorphic HC-reservoir; Kiskunhalas-NE, Pannonian Basin}, url = {https://m2.mtmt.hu/api/publication/2190426}, author = {Fiser-Nagy, Ágnes and M. Tóth, Tivadar and Vásárhelyi, Balázs and Földes, Tamás}, doi = {10.1007/s40328-012-0008-y}, journal-iso = {ACTA GEOD GEOPHYS}, journal = {ACTA GEODAETICA ET GEOPHYSICA}, volume = {48}, unique-id = {2190426}, issn = {2213-5812}, year = {2013}, eissn = {2213-5820}, pages = {53-75}, orcid-numbers = {M. Tóth, Tivadar/0000-0003-1012-1095; Vásárhelyi, Balázs/0000-0002-0568-1031} } @article{MTMT:2583272, title = {First report of Triassic vertebrate assemblages from the Villány Hills (Southern Hungary)}, url = {https://m2.mtmt.hu/api/publication/2583272}, author = {Ősi, Attila and Pozsgai, Emília and Prondvai, Edina and Botfalvai, Gábor and Götz, AE and Makádi, László and Hajdu, ZS and Csengődi, D and Czirják, G and Sebe, Krisztina and Szentesi, Zoltán}, doi = {10.1556/CEuGeol.56.2013.4.2}, journal-iso = {CENT EUR GEOL}, journal = {CENTRAL EUROPEAN GEOLOGY}, volume = {56}, unique-id = {2583272}, issn = {1788-2281}, year = {2013}, eissn = {1789-3348}, pages = {297-335}, orcid-numbers = {Ősi, Attila/0000-0003-2967-997X; Botfalvai, Gábor/0000-0002-5479-9036; Sebe, Krisztina/0000-0002-4647-2199; Szentesi, Zoltán/0000-0002-7019-5478} } @article{MTMT:23383937, title = {Understanding the kinematic evolution and genesis of a back-arc continental "sag" basin: The Neogene evolution of the Transylvanian Basin}, url = {https://m2.mtmt.hu/api/publication/23383937}, author = {Tilita, M and Matenco, L and Dinu, C and Ionescu, L and Cloetingh, S}, doi = {10.1016/j.tecto.2012.12.029}, journal-iso = {TECTONOPHYSICS}, journal = {TECTONOPHYSICS}, volume = {602}, unique-id = {23383937}, issn = {0040-1951}, year = {2013}, eissn = {1879-3266}, pages = {237-258} } @article{MTMT:24852576, title = {The evolution of a key segment in the Europe-Adria collision: The Fruska Gora of northern Serbia}, url = {https://m2.mtmt.hu/api/publication/24852576}, author = {Toljic, M and Matenco, L and Ducea, MN and Stojadinovic, U and Milivojevic, J and Deric, N}, doi = {10.1016/j.gloplacha.2012.10.009}, journal-iso = {GLOBAL PLANET CHANGE}, journal = {GLOBAL AND PLANETARY CHANGE}, volume = {103}, unique-id = {24852576}, issn = {0921-8181}, year = {2013}, eissn = {1872-6364}, pages = {39-62} } @article{MTMT:2031779, title = {Apatite as a petrogenetic indicator of Variscan granitoids in Tisza Mega-Unit (South Hungary)}, url = {https://m2.mtmt.hu/api/publication/2031779}, author = {Buda, György and Pál-Molnár, Elemér}, journal-iso = {CARPATH J EARTH ENVIRON SCI}, journal = {CARPATHIAN JOURNAL OF EARTH AND ENVIRONMENTAL SCIENCES}, volume = {7}, unique-id = {2031779}, issn = {1842-4090}, year = {2012}, eissn = {1844-489X}, pages = {47-60}, orcid-numbers = {Pál-Molnár, Elemér/0000-0002-9606-0133} } @article{MTMT:2011063, title = {Mafic enclaves in peraluminous Variscan granitoid in the Battonya Unit from Southeast Hungary}, url = {https://m2.mtmt.hu/api/publication/2011063}, author = {Buda, György and Pál-Molnár, Elemér and Koller, F}, doi = {10.4154/GC.2012.15}, journal-iso = {GEOL CROAT}, journal = {GEOLOGIA CROATICA}, volume = {65}, unique-id = {2011063}, issn = {1330-030X}, keywords = {Hungary; igneous intrusion; magmatism; mafic rock; Mica; calc alkaline rock; biotite; Micas; muscovite; granitoid; Hercynian orogeny; AMPHIBOLE; hydrothermal alteration; Feldspar; T; P; SE Hungary; secondary muscovite; primary-; I/S-type; peraluminous granitoid; basic enclave; Variscan; Depth of intrusion; enclave}, year = {2012}, eissn = {1333-4875}, pages = {243-253}, orcid-numbers = {Pál-Molnár, Elemér/0000-0002-9606-0133} } @article{MTMT:1853055, title = {Foraminifera and Ostracoda of the classic Callovian ammonite-rich bed of the Villány Mountains (Hungary)}, url = {https://m2.mtmt.hu/api/publication/1853055}, author = {Görög, Ágnes and Tóth, Emőke and Wernli, Roland}, journal-iso = {HANTKENIANA}, journal = {HANTKENIANA}, volume = {7}, unique-id = {1853055}, issn = {1219-3933}, year = {2012}, pages = {95-123}, orcid-numbers = {Görög, Ágnes/0000-0002-0910-8822; Tóth, Emőke/0000-0002-1733-7828} } @article{MTMT:1791342, title = {Influence of global, regional, and local factors on the origin of the Jurassic manganese formation in the Transdanubian Range, Hungary}, url = {https://m2.mtmt.hu/api/publication/1791342}, author = {Haas, János}, doi = {10.1016/j.oregeorev.2011.08.006}, journal-iso = {ORE GEOL REV}, journal = {ORE GEOLOGY REVIEWS}, volume = {47}, unique-id = {1791342}, issn = {0169-1368}, year = {2012}, eissn = {1872-7360}, pages = {77-86}, orcid-numbers = {Haas, János/0000-0003-0929-8889} } @article{MTMT:2421699, title = {The connection between iron ore formations and „mud-shrimp” colonizations around sunken wood debris and hydrothermal sediments in a Lower Cretaceous continental rift basin, Mecsek Mts. Hungary.}, url = {https://m2.mtmt.hu/api/publication/2421699}, author = {Jáger, Viktor and Molnár, Ferenc and Buchs, D and Kodera, P}, doi = {10.1016/j.earscirev.2012.06.003}, journal-iso = {EARTH-SCI REV}, journal = {EARTH-SCIENCE REVIEWS}, volume = {114}, unique-id = {2421699}, issn = {0012-8252}, abstract = {In the Early Cretaceous, the continental rift basin of the Mecsek Mts. (Hungary), was situated on the southern edge of the European plate. The opening of the North Atlantic Ocean created a dilatational regime that expanded to the southern edge of the European plate, where several extensional basins and submarine volcanoes were formed during the Early Cretaceous epoch. Permanent seaquake activity caused high swell events during which a large amount of terrestrial wood fragments entered into submarine canyons from rivers or suspended woods which had sunk into the deep seafloor. These fragments created extended wood-fall deposits which contributed large-scale flourishing of numerous burrowing thalassinid crustaceans. Twelve different thalassinid coprolite ichnospecies can be found in the Berriasian-Hauterivian volcanosedimentary formations. According to the seladonitic crustacean burrows which associated with framboidal pyrite containing Zoophycos and Chondrites ichnofossils (i.e. a "fodinichnia" trace fossil association), the bottom water was aerobic and the pore water was anaerobic; in the latter sulfate reduction occurred. The preservation of wood fragments around thalassinid burrows can be explained by rapid sedimentation related to turbidity currents. Due to the low temperature hydrothermal circulations of seawater, large amounts of iron were released from intrusive, pillowed basaltic sills; these sills intruded into soft, water-saturated sediments containing large amounts of thalassinid excrement. In the coprolites can be found idiomorphic mineral particles originating from the basalts, and coprolites can often be found in peperitic interpillow sediments. This indicates that the life-activity of the decapoda crustaceans in many Lower Cretaceous occurrences initially preceded the first magmatic eruptions. The paroxysm of the rift volcanism took place during the Valanginian age, when some submarine volcanoes emerged above sea level, reaching a maximum height of 300 m (above sea level); from these volcanoes further terrestrial plant debris got into the basin. Hydrothermal vents, which periodically occurred around basaltic bodies until the Hauterivian, could have contributed to the creation of favourable temperature or nutritional conditions for some decapoda crustaceans - e.g the recently described new callianassid (Nihonotrypaea thermophila), which is known only from hydrothermally infuenced habitats. Around the intrusive pillow basalts, hydrothermal circulation of oxygenated seawater occured and thick seladonitic and goethitic fills formed along the cracks and cavities of pillowed basalts. When oxidized, sulfaterich fluids passed into the crustacean coprolite-rich, reductive and anaerobic interpillow sediments, these fluids underwent an intensive sulfate reduction. Thiswas primarily due to termophil sulfate reducers which as proved by the negative sulfur isotope values (-35.9‰ and-28.0‰ δ 34S) of sulfidic hydrothermal chimneys which contain framboidal pyrite and which were formed between the pillow basalts. The largest chimney structure reached a height of 1 m, with a mass of about 150 kg. The sulfide phase is characterized by Mo enrichments up to 511 ppm. The fluid inclusion measurements fromthe calcitic precipitations of the sulfide chimneys indicate lowtemperature (~129 °C) hydrothermal activity, and the salinity of the primary fluid inclusions proves the seawater origin of the hydrothermal fluids. In some thalassinid crustacean coprolite rich interpillow sediments and in the cracks of some hydrothermal calcite, there is the presence of black, lustrous bitumine (gilsonite) which is the distillation product of hydrothermal petroleum formed mainly by the coprolites. Hydrothermal circulationsof oxygenated seawater caused subsequent oxidation of the sulfidic, interpillowsediments and chimneys; these were altered to formgoethite. Due to the short-period of the hydrothermal activity among the intrusive pillowed basalts, sulfidized interpillow sediments could not be oxidized completely. The texture of the goethitic iron ore (as an interpillow sediment) is network-like and dentritic, which is very similar to the iron-oxidic and microbial textured sediments of the Juan de Fuca Ridge. The dendritic ironoxide-hydroxide particles which were involved in this study are not hollow and exceed the size-domain characteristic for bacterial products. However, in some cases hollow- and tube-like particles having a diameter of 1.2-1.5 μm can refer to the activity of the Sphaerotilus-Leptothrix iron-oxidizer bacterial group. © 2012 Elsevier B.V.}, year = {2012}, eissn = {1872-6828}, pages = {250-278}, orcid-numbers = {Jáger, Viktor/0000-0003-1283-5198; Molnár, Ferenc/0000-0002-1873-1915} } @article{MTMT:24852889, title = {Provenance of Cretaceous synorogenic sediments from the NW Dinarides (Croatia)}, url = {https://m2.mtmt.hu/api/publication/24852889}, author = {Luzar-Oberiter, B and Mikes, T and Dunkl, István and Babic, L and von Eynatten, H}, doi = {10.1007/s00015-012-0107-3}, journal-iso = {SWISS J GEOSCI}, journal = {SWISS JOURNAL OF GEOSCIENCES}, volume = {105}, unique-id = {24852889}, issn = {1661-8726}, year = {2012}, eissn = {1661-8734}, pages = {377-399} } @article{MTMT:24852742, title = {On the formation and evolution of the Pannonian Basin: Constraints derived from the structure of the junction area between the Carpathians and Dinarides}, url = {https://m2.mtmt.hu/api/publication/24852742}, author = {Matenco, L and Radivojevic, D}, doi = {10.1029/2012TC003206}, journal-iso = {TECTONICS}, journal = {TECTONICS}, volume = {31}, unique-id = {24852742}, issn = {0278-7407}, year = {2012}, eissn = {1944-9194} } @article{MTMT:2182126, title = {Episodic sedimentation on a peri-Tethyan ridge through the Middle-Late Jurassic transition (Villany Mountains, southern Hungary)}, url = {https://m2.mtmt.hu/api/publication/2182126}, author = {Vörös, Attila}, doi = {10.1007/s10347-011-0287-8}, journal-iso = {FACIES}, journal = {FACIES}, volume = {58}, unique-id = {2182126}, issn = {0172-9179}, abstract = {The Villany area, as a central part of the Tisza microcontinent/terrane along the European margin of Tethys, was characterized by intense subsidence in the Early and Middle Triassic, followed by a long interruption of subsidence in the Late Triassic to Middle Jurassic. During the Middle-Late Jurassic transition, marine sedimentation started with three distinct sedimentary episodes dated as Late Bathonian, Early Callovian, and Middle-Late Callovian, respectively. The succession is terminated by a thick limestone of Middle Oxfordian age. The sedimentary features, microfacies, and macroinvertebrate associations of these four stratigraphic units are documented and illustrated. The Middle to Late Jurassic sedimentary episodes of the Villany succession record an interplay of local and global factors and paleogeographical changes. At the beginning, local tectonic movements governed the main features of sedimentation, though the role of eustasy was also essential. From the mid-Callovian onwards, global climatic, biotic, and paleoceanographical changes controlled the nature and formation of the local carbonate sediments. The Callovian stromatolites are attributed to the activity of sulphate-reducing bacteria in a deep sublittoral, current-swept environment. Upwelling of eutrophic Tethyan waters is recorded by the prevalence of the Bositra filament microfacies in the Callovian. The long submarine hiatus at around the Callovian-Oxfordian transition mirrors a serious restriction of the carbonate budget, due to sudden cooling and a change in the oceanic current system (opening of a circumglobal Tethyan Passage), and to a higher amount of dissolved CO2. In the Middle Oxfordian, the carbonate production considerably increased in accordance with the sudden global warming.}, year = {2012}, eissn = {1612-4820}, pages = {415-443} } @article{MTMT:1785259, title = {Petrographic, geochemical and geochronological investigation on granitic pebbles from Permotriassic metasediments of the Tisia terrain (eastern Papuk, Croatia).}, url = {https://m2.mtmt.hu/api/publication/1785259}, author = {Bisevac, V and Krenn, E and Balen, D and Finger, F and Balogh, Kadosa}, doi = {10.1007/s00710-011-0175-5}, journal-iso = {MINER PETROL}, journal = {MINERALOGY AND PETROLOGY}, volume = {102}, unique-id = {1785259}, issn = {0930-0708}, keywords = {Earth, Cosmic and Environm. Res.,}, year = {2011}, eissn = {1438-1168}, pages = {163-180} } @article{MTMT:1687934, title = {The relevance of vein texture in understanding the past hydraulic behaviour of a crystalline rock mass: reconstruction of the palaeohydrology of the Mecsekalja Zone, south Hungary}, url = {https://m2.mtmt.hu/api/publication/1687934}, author = {Dabi, Gergely and Siklósy, Zoltán and Schubert, Félix and Bajnóczi, Bernadett and M. Tóth, Tivadar}, doi = {10.1111/j.1468-8123.2011.00342.x}, journal-iso = {GEOFLUIDS}, journal = {GEOFLUIDS}, volume = {11}, unique-id = {1687934}, issn = {1468-8115}, year = {2011}, eissn = {1468-8123}, pages = {309-327}, orcid-numbers = {Schubert, Félix/0000-0001-8647-5354; Bajnóczi, Bernadett/0000-0003-0006-7611; M. Tóth, Tivadar/0000-0003-1012-1095} }