@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:31382822,
	title = {Halorina cryptica nov. ichnogen., nov. ichnosp., mass-occurrence of Upper Triassic crustacean microcoprolites from neptunian dikes and sills cutting the Dachstein-type carbonate platform and their paleoenvironmental significance (Northern Apuseni Mountains, Romania)},
	url = {https://m2.mtmt.hu/api/publication/31382822},
	author = {Lazăr, Iuliana and Schlagintweit, Felix and Grădinaru, Eugen},
	doi = {10.1016/j.geobios.2020.06.003},
	journal-iso = {GEOBIOS-LYON},
	journal = {GEOBIOS},
	volume = {61},
	unique-id = {31382822},
	issn = {0016-6995},
	year = {2020},
	eissn = {1777-5728},
	pages = {31-39},
	orcid-numbers = {Grădinaru, Eugen/0000-0003-3445-7853}
}

@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: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: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: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: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:3385746,
	title = {„Oázis a sivatagban” — különösen gazdag ősmaradvány-együttes a fosszíliaszegény üllési Szegedi Dolomitból},
	url = {https://m2.mtmt.hu/api/publication/3385746},
	author = {Szurominé, Korecz Andrea and Garaguly, István and Szente, István and Raucsikné Varga, Andrea Beáta and Raucsik, Béla},
	doi = {10.23928/foldt.kozl.2018.148.2.119},
	journal-iso = {FÖLDTANI KÖZLÖNY},
	journal = {FÖLDTANI KÖZLÖNY},
	volume = {148},
	unique-id = {3385746},
	issn = {0015-542X},
	year = {2018},
	eissn = {2559-902X},
	pages = {119-124},
	orcid-numbers = {Garaguly, István/0000-0002-2802-0738; Raucsikné Varga, Andrea Beáta/0000-0002-8673-1482; Raucsik, Béla/0000-0002-1951-5974}
}

@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: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}
}

@inproceedings{MTMT:25316462,
	title = {Opportunities for environmental impact assessment of the geothermal area beiu},
	url = {https://m2.mtmt.hu/api/publication/25316462},
	author = {Cəlburean, R and Codrea, VA and Barbu, O},
	booktitle = {24th International Mining Congress of Turkey, IMCET 2015},
	publisher = {TMMOB Chamber of Mining Engineers},
	unique-id = {25316462},
	year = {2015},
	pages = {1480-1485}
}

@{MTMT:32071291,
	title = {Geological and Tectonic Background},
	url = {https://m2.mtmt.hu/api/publication/32071291},
	author = {Haas, János},
	booktitle = {Landscapes and Landforms of Hungary},
	doi = {10.1007/978-3-319-08997-3_2},
	unique-id = {32071291},
	abstract = {The Pannonian region (the Pannonian or Carpathian Basin and the surrounding mountain ranges) is part of the Mediterranean Mountain System, which was formed during the last plate-tectonic cycle since the latest Paleozoic times. In Europe it is an about 300–800Â km wide belt (Neo-Europe) accreted to the previously consolidated parts of Europe (Hercynian/Variscan Europe or Meso-Europe) as a result of the Alpine orogeny caused by convergence of the European (Eurasian) and African Plates. The present-day geological structure of the region is mostly determined by the evolution of the Tethys and Atlantic Ocean systems, i.e. the dismembering of the European and African continental plate margins during the early evolutionary stages and their tectonic deformation and uplifting as consequences of plate and microplate collisions. Plate-tectonic processes led to the formation of the large Pannonian Basin in the Late Cenozoic times. Hungary lies in the central part of the Pannonian Basin that is actually a system of several basins separated by isolated ranges of Palaeozoic and Mesozoic, sedimentary, magmatic and metamorphic formations and Cenozoic sedimentary and igneous rocks. © 2015, Springer International Publishing Switzerland.},
	keywords = {Pannonian Basin; plate tectonics; Tisza Megaunit; ALCAPA Megaunit},
	year = {2015},
	pages = {7-17},
	orcid-numbers = {Haas, János/0000-0003-0929-8889}
}

@article{MTMT:3089130,
	title = {Sideritic-kaolinitic and green clay layers in the Mecsek Mountains (SW Hungary): Indicators of Middle Triassic volcanism-myth or reality?},
	url = {https://m2.mtmt.hu/api/publication/3089130},
	author = {Lukoczki, Georgina and Budai, Tamás and Németh, Tibor},
	doi = {10.1556/24.58.2015.4.4},
	journal-iso = {CENT EUR GEOL},
	journal = {CENTRAL EUROPEAN GEOLOGY},
	volume = {58},
	unique-id = {3089130},
	issn = {1788-2281},
	year = {2015},
	eissn = {1789-3348},
	pages = {334-355},
	orcid-numbers = {Lukoczki, Georgina/0000-0002-0661-0198; Németh, Tibor/0000-0002-1836-6006}
}

@article{MTMT:2943291,
	title = {The origin of the Avram Iancu U–Ni–Co–Bi–As mineralization, Ba˘iţa (Bihor) metallogenic district, Bihor Mts., Romania},
	url = {https://m2.mtmt.hu/api/publication/2943291},
	author = {Zajzon, Norbert and Szentpéteri, K and Szakáll, Sándor and Kristály, Ferenc},
	doi = {10.1007/s00531-015-1175-1},
	journal-iso = {INT J EARTH SCI},
	journal = {INTERNATIONAL JOURNAL OF EARTH SCIENCES},
	volume = {104},
	unique-id = {2943291},
	issn = {1437-3254},
	year = {2015},
	eissn = {1437-3262},
	pages = {1865-1887},
	orcid-numbers = {Kristály, Ferenc/0000-0002-0075-5994}
}

@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:2586947,
	title = {A monyoródi jura mészkő és miocén konglomerátum feltárás értékelése a földtudományi természetvédelem szempontjából},
	url = {https://m2.mtmt.hu/api/publication/2586947},
	author = {Hágen, András},
	journal-iso = {TÁJÖKOLÓGIAI LAPOK / J LANDSCAPE ECOL},
	journal = {TÁJÖKOLÓGIAI LAPOK / JOURNAL OF LANDSCAPE ECOLOGY},
	volume = {12},
	unique-id = {2586947},
	issn = {1589-4673},
	year = {2014},
	pages = {173-182}
}

@article{MTMT:25316463,
	title = {Microbial-dominated carbonate platforms during the Ladinian rifting: Sequence stratigraphy and evolution of accommodation in a fault-controlled setting (Catalan Coastal Ranges, NE Spain)},
	url = {https://m2.mtmt.hu/api/publication/25316463},
	author = {Mercedes-Martín, R and Salas, R and Arenas, C},
	doi = {10.1111/bre.12026},
	journal-iso = {BASIN RES},
	journal = {BASIN RESEARCH},
	volume = {26},
	unique-id = {25316463},
	issn = {0950-091X},
	year = {2014},
	eissn = {1365-2117},
	pages = {269-296}
}

@article{MTMT:27620817,
	title = {A Triassic homoclinal ramp from the Western Tethyan realm, Western Balkanides, Bulgaria: Integrated insight with special emphasis on the Anisian outer to inner ramp facies transition},
	url = {https://m2.mtmt.hu/api/publication/27620817},
	author = {Chatalov, A},
	doi = {10.1016/j.palaeo.2013.04.028},
	journal-iso = {PALAEOGEOGR PALAEOCL},
	journal = {PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY},
	volume = {386},
	unique-id = {27620817},
	issn = {0031-0182},
	year = {2013},
	eissn = {1872-616X},
	pages = {34-58}
}

@inproceedings{MTMT:25316466,
	title = {Geothermal energy in Western Apuseni Mountains (Romania) for economic and sustainable purposes},
	url = {https://m2.mtmt.hu/api/publication/25316466},
	author = {Codrea, V and Cälburean, R},
	booktitle = {23rd International Mining Congress and Exhibition of Turkey, IMCET 2013},
	publisher = {TMMOB Maden Mühendisleri Odası},
	unique-id = {25316466},
	year = {2013},
	pages = {1707-1712}
}

@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}
}

@book{MTMT:2048748,
	title = {Geology of Hungary},
	url = {https://m2.mtmt.hu/api/publication/2048748},
	isbn = {9783642219092},
	doi = {10.1007/978-3-642-21910-8},
	editor = {Haas, János},
	publisher = {Springer Netherlands},
	unique-id = {2048748},
	year = {2013},
	orcid-numbers = {Haas, János/0000-0003-0929-8889}
}

@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:2048753,
	title = {Climatic controls on sedimentary environments in the Triassic of the Transdanubian Range (Western Hungary)},
	url = {https://m2.mtmt.hu/api/publication/2048753},
	author = {Haas, János and Budai, Tamás and Raucsik, Béla},
	doi = {10.1016/j.palaeo.2012.06.031},
	journal-iso = {PALAEOGEOGR PALAEOCL},
	journal = {PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY},
	volume = {353-355},
	unique-id = {2048753},
	issn = {0031-0182},
	year = {2012},
	eissn = {1872-616X},
	pages = {31-44},
	orcid-numbers = {Haas, János/0000-0003-0929-8889; Raucsik, Béla/0000-0002-1951-5974}
}

@inbook{MTMT:1982402,
	title = {Geological and Tectonic setting},
	url = {https://m2.mtmt.hu/api/publication/1982402},
	author = {Haas, János},
	booktitle = {Recent landform evolution},
	doi = {10.1007/978-94-007-2448-8_1},
	unique-id = {1982402},
	year = {2012},
	pages = {3-18},
	orcid-numbers = {Haas, János/0000-0003-0929-8889}
}

@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:2030780,
	title = {Structural formation of Tisza and Száva-Bükk units in the Lower Cretaceous period. A Tisza és a száva-bükki egység szerkezetének alsó-krétabeli alakulása},
	url = {https://m2.mtmt.hu/api/publication/2030780},
	author = {Posgay, Károly and Bodoky, Tamás János and Falus, György and Kovács, István János and Madarasi, András and Gúthy, Tibor and Hegedűs, Endre and Kovács, Attila Csaba},
	journal-iso = {MAGYAR GEOFIZIKA},
	journal = {MAGYAR GEOFIZIKA},
	volume = {52},
	unique-id = {2030780},
	issn = {0025-0120},
	abstract = {Comparing the deep refl ection seismic profi les (PGT-1, ÉK-2) measured along the Hungarian Geotraverse with geological, magnetotelluric and geochemical data we came to the conclusion that on the surface of the Pre-Cenozoic basement there is a sequence of rocks which is repeated several times along the Geotraverse. That sequence is composed of metamorphic rocks and of Triassic, Jurassic and Cretaceous beds superimposed on them with SSE line of dip and forming belts with SWW-NEE strike. Rows of characteristic refl ections can be observed which are started at the edges of the belts and run along zones of the section sloping towards the SSE part of the profi le. From those dislocation zones can be deduced, which divide the investigated part of Tisza unit into thick plate like blocks. This lithosphere structure might be formed when a branch of the Vardar Ocean (which joined to the Száva-Bükk unit) was pushed under the Tisza unit about during the Lower Cretaceous. The Pre-Cenozoic basement is intersected by the subduction surface along the Mid-Hungarian Line (at least nearby the Hungarian Geotravers). This idea is backed up by the followings: - Those refl ections which are parallel to the dislocation belt starting in the vicinity of the Mid-Hungarian Line and slope towards SSE indicate displacement surfaces. - On the Northern part of the Geotravers (ÉK-2 section) the continuations of these refl ections bend into horizontal direction. From that we may conclude a NNW directional decrease of the sloping of the plate, namely the nearly horizontal part of the plate subducting in SSE direction. - On that upper part of the subducting plate a low resistivity zone revealed by magnetotellurics can be followed to large depth. Presumably this zone sloping SSE indicates a higher water content of the plate which might be bound in chain silicates (amphiboles and micas). The results of our investigation show that on the studied part of the Tisza unit the structure of the thick plate under the flysch is similar to those of its other parts along the Hungarian Geotraverse, namely under the flysch from NNW to SSE crystalline rocks and Triassic, Jurassic and Cretaceous beds superimposed on them can be found. It is conceivable that those layers got into a depth of CH generation protected by flysch. © 2011 Magyar Geofi zikusok Egyesülete.},
	keywords = {water content; Cretaceous; subduction zone; geochemical method; lithosphere; Micas; Tisza river; Triassic; Electrical resistivity; Jurassic; metamorphic rock; Axios River; seismic reflection; plate motion; magnetotelluric method; flysch; crystalline rock; geofizika},
	year = {2011},
	eissn = {2677-1497},
	pages = {135-150},
	orcid-numbers = {Kovács, István János/0000-0002-3488-3716}
}

@article{MTMT:1537934,
	title = {Speleothems and pine trees as sensitive indicators of environmental pollution - A case study of the effect of uranium-ore mining in Hungary},
	url = {https://m2.mtmt.hu/api/publication/1537934},
	author = {Siklósy, Zoltán and Kern, Zoltán and Demény, Attila and Pilet, S and Leél-Őssy, Szabolcs and Lin, K and Shen, CC and Kovács-Széles, Éva and Breitner, Dániel},
	doi = {10.1016/j.apgeochem.2011.01.025},
	journal-iso = {APPL GEOCHEM},
	journal = {APPLIED GEOCHEMISTRY},
	volume = {26},
	unique-id = {1537934},
	issn = {0883-2927},
	year = {2011},
	eissn = {1872-9134},
	pages = {666-678},
	orcid-numbers = {Kern, Zoltán/0000-0003-4900-2587; Demény, Attila/0000-0003-0522-9018; Leél-Őssy, Szabolcs/0000-0002-5548-129X}
}

@article{MTMT:1791284,
	title = {Tectonostratigraphic terranes and zones juxtaposed along the Mid-Hungarian Line: their contrasting evolution and relationships},
	url = {https://m2.mtmt.hu/api/publication/1791284},
	author = {Kovács, S and Buda, György and Haas, János and Brezsnyánszky, Károly and Harangi, Szabolcs},
	doi = {10.1556/CEuGeol.53.2010.2-3.4},
	journal-iso = {CENT EUR GEOL},
	journal = {CENTRAL EUROPEAN GEOLOGY},
	volume = {53},
	unique-id = {1791284},
	issn = {1788-2281},
	keywords = {Hungary; Pannonian Basin; Neogene; Miocene; Correlation; tectonostratigraphy; terrane; Hercynian orogeny; Variscan evolution; tectonostratigraphic terranes; Mid-Hungarian Zone; Mid-Hungarian Line; Mecsek Zone; Alpine evolution},
	year = {2010},
	eissn = {1789-3348},
	pages = {165-180},
	orcid-numbers = {Haas, János/0000-0003-0929-8889; Harangi, Szabolcs/0000-0003-2372-4581}
}

@article{MTMT:27640170,
	title = {Microtectonic measurements and interpretation of the Mesozoic formations in the Villány Hills and Görcsöny- Máriakéménd Ridge, Hungary},
	url = {https://m2.mtmt.hu/api/publication/27640170},
	author = {Petrik, Attila},
	doi = {10.1556/CEuGeol.53.2010.1.2},
	journal-iso = {CENT EUR GEOL},
	journal = {CENTRAL EUROPEAN GEOLOGY},
	volume = {53},
	unique-id = {27640170},
	issn = {1788-2281},
	abstract = {In the framework of a National Research Fond project varied scientific investigations
		are being carried out with the aim of preparing a comprehensive paleogeographical
		reconstruction of the Tisza structural unit. I have joined this project and performed
		microtectonical measurements in the area of the Villány Hills and Görcsöny-
		Máriakéménd Ridge. A lot of publications and theses have already been made about
		the structural development of the Mecsek-Villány area (CSONTOS & BERGERAT 1988;
		BENKOVICS 1997; CSONTOS ET. AL 2002), but the Villány Hills and their environments
		were in a shade role contrary to the Mecsek Mountains in them. The task was to
		establish the delimitation the phases of structural transformation and determine their
		relative and numeric ages. It has been an important issue to clarify how far the events
		of structural transformation postulated by me can be integrated into the regional
		geological processes. The tectonical conditions of the area at issue have been
		analysed relying upon some stereographical projections, figures and models. In
		addition describing the structural elements of the 12 quarries investigated in the study
		demonstrates the related stress fields as well. Seven Villány-, and five Görcsöny-
		Máriakéménd quarries, the data of over 700 striations, 600 lythoclases, various plastic
		deformation elements (folds, flexures) as well as stylolites were recorded. It was an
		important issue to integrate those structural elements into the regional geological
		processes which didn’t show any significant movements. Based on the data recorded
		the structural, paleotectonic conditions of the studied area were determined.},
	year = {2010},
	eissn = {1789-3348},
	pages = {21-42}
}

@article{MTMT:1417437,
	title = {A villányi mezozoos rétegsor: visszatekintés új nézőpontból [The Mesozoic sedimentary sequences at Villány (southern Hungary)]},
	url = {https://m2.mtmt.hu/api/publication/1417437},
	author = {Vörös, Attila},
	journal-iso = {FÖLDTANI KÖZLÖNY},
	journal = {FÖLDTANI KÖZLÖNY},
	volume = {140},
	unique-id = {1417437},
	issn = {0015-542X},
	year = {2010},
	eissn = {2559-902X},
	pages = {3-30}
}

@article{MTMT:1417445,
	title = {Tectonically-controlled Late Triassic and Jurassic sedimentary cycles on a peri-Tethyan ridge (Villány, southern Hungary).},
	url = {https://m2.mtmt.hu/api/publication/1417445},
	author = {Vörös, Attila},
	doi = {10.1556/CEuGeol.52.2009.2.2},
	journal-iso = {CENT EUR GEOL},
	journal = {CENTRAL EUROPEAN GEOLOGY},
	volume = {52},
	unique-id = {1417445},
	issn = {1788-2281},
	year = {2009},
	eissn = {1789-3348},
	pages = {125-151}
}

@article{MTMT:32550094,
	title = {Triassic},
	url = {https://m2.mtmt.hu/api/publication/32550094},
	author = {Feist-Burkhardt, S and Götz, AE and Szulc, J and Borkhataria, R and Geluk, M and Haas, János and Hornung, J and Jordan, P and Kempf, O and Michalík, J and Nawrocki, J and Reinhardt, L and Ricken, W and Röhling, HG and Rüffer, T and Török, Ákos and Zühlke, R},
	journal-iso = {CENTRAL EUROPE},
	journal = {CENTRAL EUROPE},
	volume = {2},
	unique-id = {32550094},
	issn = {1479-0963},
	year = {2008},
	eissn = {1745-8218},
	pages = {749-821},
	orcid-numbers = {Haas, János/0000-0003-0929-8889; Török, Ákos/0000-0002-5394-4510}
}

@article{MTMT:20754329,
	title = {Metallogeny of the Northwestern and Central Dinarides and Southern Tisia},
	url = {https://m2.mtmt.hu/api/publication/20754329},
	author = {Palinkas, LA and Sostaric, SB and Palinkas, SS},
	doi = {10.1016/j.oregeorev.2008.05.006},
	journal-iso = {ORE GEOL REV},
	journal = {ORE GEOLOGY REVIEWS},
	volume = {34},
	unique-id = {20754329},
	issn = {0169-1368},
	year = {2008},
	eissn = {1872-7360},
	pages = {501-520}
}

@article{MTMT:1247526,
	title = {Palynology of a terrestrial coal-bearing series across the Triassic/Jurassic boundary (Mecsek Mts, Hungary)},
	url = {https://m2.mtmt.hu/api/publication/1247526},
	author = {Ruckwied, K and Götz, A and Pálfy, József and Török, Ákos},
	doi = {10.1556/CEuGeol.51.2008.1.1},
	journal-iso = {CENT EUR GEOL},
	journal = {CENTRAL EUROPEAN GEOLOGY},
	volume = {51},
	unique-id = {1247526},
	issn = {1788-2281},
	year = {2008},
	eissn = {1789-3348},
	pages = {1-15},
	orcid-numbers = {Pálfy, József/0000-0001-9686-1849; Török, Ákos/0000-0002-5394-4510}
}

@article{MTMT:25730251,
	title = {The Alpine-Carpathian-Dinaridic orogenic system: correlation and evolution of tectonic units},
	url = {https://m2.mtmt.hu/api/publication/25730251},
	author = {Schmid, Stefan M and Bernoulli, Daniel and Fuegenschuh, Bernhard and Matenco, Liviu and Schefer, Senecio and Schuster, Ralf and Tischler, Matthias and Ustaszewski, Kamil},
	doi = {10.1007/s00015-008-1247-3},
	journal-iso = {SWISS J GEOSCI},
	journal = {SWISS JOURNAL OF GEOSCIENCES},
	volume = {101},
	unique-id = {25730251},
	issn = {1661-8726},
	year = {2008},
	eissn = {1661-8734},
	pages = {139-183}
}

@article{MTMT:152181,
	title = {Facies pattern of western Tethyan Middle Triassic black carbonates: The example of Gutenstein Formation in Silica Nappe, Carpathians, Hungary, and its correlation to formations of adjoining areas.},
	url = {https://m2.mtmt.hu/api/publication/152181},
	author = {Hips, Kinga},
	doi = {10.1016/j.sedgeo.2006.05.001},
	journal-iso = {SEDIMENT GEOL},
	journal = {SEDIMENTARY GEOLOGY},
	volume = {194},
	unique-id = {152181},
	issn = {0037-0738},
	year = {2007},
	eissn = {1879-0968},
	pages = {99-114},
	orcid-numbers = {Hips, Kinga/0000-0003-2315-120X}
}

@article{MTMT:2247784,
	title = {A CEL07 mélyszeizmikus szelvény újraértékelése [Reinterpretation of CEL07 deep seismic profile]},
	url = {https://m2.mtmt.hu/api/publication/2247784},
	author = {Posgay, Károly and Kovács, Attila Csaba and Csabafi, Róbert Imre and Bodoky, Tamás János and Hegedűs, Endre and Fancsik, Tamás and Riegler, Balázs},
	journal-iso = {MAGYAR GEOFIZIKA},
	journal = {MAGYAR GEOFIZIKA},
	volume = {48},
	unique-id = {2247784},
	issn = {0025-0120},
	keywords = {geofizika; CEL},
	year = {2007},
	eissn = {2677-1497},
	pages = {87-98}
}

@article{MTMT:24849130,
	title = {Generation of normal and adakite-like calc-alkaline magmas in a non-subductional environment: An Sr-O-H isotopic study of the Apuseni Mountains neogene magmatic province, Romania},
	url = {https://m2.mtmt.hu/api/publication/24849130},
	author = {Seghedi, I and Bojar, AV and Downes, H and Emilian, R and Tonarini, S and Mason, P},
	doi = {10.1016/j.chemgeo.2007.07.027},
	journal-iso = {CHEM GEOL},
	journal = {CHEMICAL GEOLOGY},
	volume = {245},
	unique-id = {24849130},
	issn = {0009-2541},
	year = {2007},
	eissn = {1872-6836},
	pages = {70-88}
}

@article{MTMT:152226,
	title = {Conodont colour alteration related to a half-graben structure: an example from the Mesozoic of the Mecsek and Villány Hills area (Tisza Megaunit, Southern Hungary)},
	url = {https://m2.mtmt.hu/api/publication/152226},
	author = {Kovács, Sándor and Rálisch-Felgenhauer, E and Bóna, J},
	journal-iso = {GEOL CARPATH},
	journal = {GEOLOGICA CARPATHICA},
	volume = {57},
	unique-id = {152226},
	issn = {1335-0552},
	year = {2006},
	eissn = {1336-8052},
	pages = {257-268}
}

@article{MTMT:21491493,
	title = {Geology of the Lower Triassic Jakabhegy Sandstone Formation, Hungary, SE Transdanubia.},
	url = {https://m2.mtmt.hu/api/publication/21491493},
	author = {Barabás, A and Barabás-Stuhl, Á},
	doi = {10.1556/ageol.48.2005.1.1},
	journal-iso = {ACTA GEOL HUNG},
	journal = {ACTA GEOLOGICA HUNGARICA: A QUARTERLY OF THE HUNGARIAN ACADEMY OF SCIENCES},
	volume = {48},
	unique-id = {21491493},
	issn = {0236-5278},
	year = {2005},
	pages = {1-47}
}

@book{MTMT:1449021,
	title = {Magyarország és környezetének regionális földtana 1.. Paleozoikum-paleogén},
	url = {https://m2.mtmt.hu/api/publication/1449021},
	isbn = {9634637442},
	author = {Császár, Géza},
	publisher = {ELTE Eötvös Kiadó Kft.},
	unique-id = {1449021},
	year = {2005}
}

@article{MTMT:27161018,
	title = {Middle Anisian (Pelsonian) platform conodonts from the Triassic of the Mecsek Mts (South Hungary) - Their taxonomy and stratigraphic significance},
	url = {https://m2.mtmt.hu/api/publication/27161018},
	author = {Kovács, Sándor and Rálisch-Felgenhauer, E},
	doi = {10.1556/AGeol.48.2005.1.3},
	journal-iso = {ACTA GEOL HUNG},
	journal = {ACTA GEOLOGICA HUNGARICA: A QUARTERLY OF THE HUNGARIAN ACADEMY OF SCIENCES},
	volume = {48},
	unique-id = {27161018},
	issn = {0236-5278},
	year = {2005},
	pages = {69-105}
}

@article{MTMT:21491542,
	title = {Middle Anisian (Pelsonian) platform conodonts from the Triassic of the Villány Hills, South Hungary},
	url = {https://m2.mtmt.hu/api/publication/21491542},
	author = {Kovács, Sándor and Bóna, J and Rálisch-Felgenhauer, E},
	doi = {10.1556/AGeol.48.2005.1.4},
	journal-iso = {ACTA GEOL HUNG},
	journal = {ACTA GEOLOGICA HUNGARICA: A QUARTERLY OF THE HUNGARIAN ACADEMY OF SCIENCES},
	volume = {48},
	unique-id = {21491542},
	issn = {0236-5278},
	year = {2005},
	pages = {107-115}
}

@article{MTMT:1236932,
	title = {Mesozoic plate tectonic reconstruction of the carpathian region},
	url = {https://m2.mtmt.hu/api/publication/1236932},
	author = {Csontos, L and Vörös, Attila},
	doi = {10.1016/j.palaeo.2004.02.033},
	journal-iso = {PALAEOGEOGR PALAEOCL},
	journal = {PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY},
	volume = {210},
	unique-id = {1236932},
	issn = {0031-0182},
	abstract = {Palaeomagnetic, palaeobiogeographic and structural comparisons of
		different parts of the Alpine-Carpathian region suggest that four
		terranes comprise this area: the Alcapa, Tisza, Dacia and Adria
		terranes. These terranes are composed of different Mesozoic continental
		and oceanic fragments that were each assembled during a complex Late
		Jurassic-Cretaceous Palaeogene history. Palaeomagnetic and tectonic
		data suggest that the Carpathians are built up by two major oroclinal
		bends. The Alcapa bend has the Meliata oceanic unit, correlated with
		the Dinaric Vardar ophiolite, in its core. It is composed of the
		Western Carpathians, Eastern Alps and Southern Alcapa units
		(Transdanubian Range, Bukk). This terrane finds its continuation in the
		High Karst margin of the Dinarides. Further elements of the Alcapa
		terrane are thought to be derived from collided microcontinents:
		Czorsztyn in the N and a carbonate unit (Tisza?) in the SE. The
		Tisza-Dacia bend has the Vardar oceanic unit in its core. It is
		composed of the Bihor and Getic microcontinents. This terrane finds its
		continuation in the Serbo-Macedonian Massif of the Balkans.
		The Bihor-Getic microcontinent originally laid east of the Western
		Carpathians and filled the present Carpathian embayment in the Late
		Palaeozoic-Early Mesozoic. The Vardar ocean occupied an intermediate
		position between the Western Carpathian-Austroalpine-Transdanubian-High
		Karst margin and the Bihor-Getic-Serbo-Macedonian microcontinent. The
		Vardar and Pindos oceans were opened in the heart of the
		Mediterranean-Adriatic microcontinent in the Late Permian-Middle
		Triassic. Vardar subducted by the end of Jurassic, causing the
		Bihor-Getic-Serbo-Macedonian microcontinent to collide with the
		internal Dinaric-Western Carpathian margin.
		An external Penninic-Vahic ocean tract began opening in the Early
		Jurassic, separating the Austroalpine-Western Carpathian microcontinent
		(and its fauna) from the European shelf. Further east, the
		Severin-Ceahlau-Magura also began opening in the Early Jurassic, but
		final separation of the Bihor-Getic ribbon (and its fauna) from the
		European shelf did not take place until the late Middle Jurassic.
		The Alcapa and the Tisza-Dacia were bending during the
		Albian-Maastrichtian. The two oroclinal bends were finally opposed and
		pushed into the gates of the Carpathian embayment during the Palaeogene
		and Neogene. At that time, the main NS shortening in distant Alpine and
		Hellenic sectors was linked by a broader right-lateral shear zone along
		the former Vardar suture. (C) 2004 Elsevier B.V. All rights reserved.},
	year = {2004},
	eissn = {1872-616X},
	pages = {1-56}
}

@article{MTMT:1019054,
	title = {Mesozoic evolution of the Tisza Mega-unit},
	url = {https://m2.mtmt.hu/api/publication/1019054},
	author = {Haas, János and Péró, Csaba},
	doi = {10.1007/s00531-004-0384-9},
	journal-iso = {INT J EARTH SCI},
	journal = {INTERNATIONAL JOURNAL OF EARTH SCIENCES},
	volume = {93},
	unique-id = {1019054},
	issn = {1437-3254},
	year = {2004},
	eissn = {1437-3262},
	pages = {297-313},
	orcid-numbers = {Haas, János/0000-0003-0929-8889}
}

@article{MTMT:1855086,
	title = {Geochemistry and petrogenesis of Early Cretaceous alkaline igneous rocks in Central Europe: implications for a long-lived EAR-type mantle component beneath Europe.},
	url = {https://m2.mtmt.hu/api/publication/1855086},
	author = {Harangi, Szabolcs and Tonarini, S and Vaselli, O and Manetti, P},
	doi = {10.1556/AGeol.46.2003.1.6},
	journal-iso = {ACTA GEOL HUNG},
	journal = {ACTA GEOLOGICA HUNGARICA: A QUARTERLY OF THE HUNGARIAN ACADEMY OF SCIENCES},
	volume = {46},
	unique-id = {1855086},
	issn = {0236-5278},
	year = {2003},
	pages = {77-94},
	orcid-numbers = {Harangi, Szabolcs/0000-0003-2372-4581}
}

@article{MTMT:22242043,
	title = {Geodynamics of SW-Pannonian inselbergs (Mecsek and Villány Mts, SW Hungary): Inferences from a complex structural analysis},
	url = {https://m2.mtmt.hu/api/publication/22242043},
	author = {Csontos, L and Márton, E and Wórum, G and Benkovics, L},
	journal-iso = {EGU STEPHAN MUELLER SPEC PUBL SER},
	journal = {EGU STEPHAN MUELLER SPECIAL PUBLICATION SERIES},
	volume = {3},
	unique-id = {22242043},
	issn = {1868-4556},
	year = {2002},
	eissn = {1868-4564},
	pages = {227-245}
}

@article{MTMT:2899890,
	title = {Tertiary deformation history from seismic section study and fault analysis in a former European Tethyan margin (the Mecsek-Villany area, SW Hungary)},
	url = {https://m2.mtmt.hu/api/publication/2899890},
	author = {Csontos, László and Benkovics, L and Bergerat, F and Mansy, JL and Worum, G},
	doi = {10.1016/S0040-1951(02)00363-3},
	journal-iso = {TECTONOPHYSICS},
	journal = {TECTONOPHYSICS},
	volume = {357},
	unique-id = {2899890},
	issn = {0040-1951},
	abstract = {Outcrop-scale structural data and seismic section interpretation are combined to unveil a very complicated Tertiary deformation history of a once Tethyan margin: the Mecsek-Villany area of Hungary. This combination of data helped to reconstruct the possible activity of individual fault zones. At least four ENE-WSW striking zones-the Northern Imbricates, the South Mecsek zone, the Gorcsony-Mariakemend ridge and the Villany Mountains-were confirmed as regional long-lived transpressive zones with very complicated internal deformation, frequently with oppositely dipping thrust faults. Tertiary structural history began with a roughly N-S-directed shortening in the South Mecsek zone. It was followed by a NE-SW-directed transpression activating practically all important wrench zones together with perpendicular transfer faults. Basins were created along some of these deformation zones, but were also affected by major tilts due to inversion. After a relatively quiescent period in the Middle Miocene, the Late Sarmatian inversion followed. Shortly after, this event was relayed by a NE-SW-directed extension-transtension. An important inversion period characterised by NW-SE compression occurred in Late Pannonian (Messinian), when all the former wrench zones were reactivated as right-lateral shear. This event is responsible for the present topography of the region. (C) 2002 Elsevier Science B.V. All rights reserved.},
	year = {2002},
	eissn = {1879-3266},
	pages = {81-102}
}

@article{MTMT:152249,
	title = {Lower Triassic shallow marine succession in the Bükk Mountains, NE Hungary},
	url = {https://m2.mtmt.hu/api/publication/152249},
	author = {Hips, Kinga and Pelikán, P},
	journal-iso = {GEOL CARPATH},
	journal = {GEOLOGICA CARPATHICA},
	volume = {53},
	unique-id = {152249},
	issn = {1335-0552},
	year = {2002},
	eissn = {1336-8052},
	pages = {351-367},
	orcid-numbers = {Hips, Kinga/0000-0003-2315-120X}
}

@article{MTMT:21491550,
	title = {Caves formed within Upper Cretaceous skarns at Bǎiţa Bihor County, Romania: Mineral deposition and speleogenesis},
	url = {https://m2.mtmt.hu/api/publication/21491550},
	author = {Onac, B P},
	doi = {10.2113/gscanmin.40.6.1693},
	journal-iso = {CAN MINERAL},
	journal = {CANADIAN MINERALOGIST},
	volume = {40},
	unique-id = {21491550},
	issn = {0008-4476},
	year = {2002},
	eissn = {1499-1276},
	pages = {1693-1703}
}

@article{MTMT:20045897,
	title = {Kinematics of the Alpine-West Carpathian orogen and palaeogeographic implications},
	url = {https://m2.mtmt.hu/api/publication/20045897},
	author = {Neugebauer, J and Greiner, B and Appel, E},
	doi = {10.1144/jgs.158.1.97},
	journal-iso = {J GEOL SOC LONDON},
	journal = {JOURNAL OF THE GEOLOGICAL SOCIETY},
	volume = {158},
	unique-id = {20045897},
	issn = {0016-7649},
	year = {2001},
	eissn = {2041-479X},
	pages = {97-110}
}

@article{MTMT:1098540,
	title = {Alpine low-T prograde metamorphism in the post-Variscan basement of the Great Plain, Tisza Unit (Pannonian Basin, Hungary)},
	url = {https://m2.mtmt.hu/api/publication/1098540},
	author = {Árkai, Péter and Bérczi, Makk A and Balogh, Kadosa},
	journal-iso = {ACTA GEOL HUNG},
	journal = {ACTA GEOLOGICA HUNGARICA: A QUARTERLY OF THE HUNGARIAN ACADEMY OF SCIENCES},
	volume = {43},
	unique-id = {1098540},
	issn = {0236-5278},
	year = {2000},
	pages = {43-63}
}

@article{MTMT:152233,
	title = {Tectonostratigraphic terranes in the pre-Neogene basement of the Hungarian part of the Pannonian area},
	url = {https://m2.mtmt.hu/api/publication/152233},
	author = {Kovács, Sándor and Szederkényi, T and Haas, János and Buda, György and Császár, Géza and Nagymarosy, András},
	journal-iso = {ACTA GEOL HUNG},
	journal = {ACTA GEOLOGICA HUNGARICA: A QUARTERLY OF THE HUNGARIAN ACADEMY OF SCIENCES},
	volume = {43},
	unique-id = {152233},
	issn = {0236-5278},
	year = {2000},
	pages = {225-328},
	orcid-numbers = {Haas, János/0000-0003-0929-8889}
}

@article{MTMT:1635943,
	title = {Formation of dolomite mottling in Middle Triassic ramp carbonates (Southern Hungary)},
	url = {https://m2.mtmt.hu/api/publication/1635943},
	author = {Török, Ákos},
	doi = {10.1016/S0037-0738(99)00137-2},
	journal-iso = {SEDIMENT GEOL},
	journal = {SEDIMENTARY GEOLOGY},
	volume = {131},
	unique-id = {1635943},
	issn = {0037-0738},
	year = {2000},
	eissn = {1879-0968},
	pages = {131-145},
	orcid-numbers = {Török, Ákos/0000-0002-5394-4510}
}

@article{MTMT:22874257,
	title = {The Triassic of the Alps and Carpathians and its interregional correlation},
	url = {https://m2.mtmt.hu/api/publication/22874257},
	author = {Vörös, Attila},
	doi = {10.1016/S0920-5446(00)80011-4},
	journal-iso = {DEVEL PALAEONT STRATIGR},
	journal = {DEVELOPMENTS IN PALAEONTOLOGY AND STRATIGRAPHY},
	volume = {18},
	unique-id = {22874257},
	issn = {0920-5446},
	abstract = {The Triassic stratigraphy and facies of the four major terranes of the Alpine-Carpathian region is shortly described and illustrated by schematic stratigraphic charts. The main stratigraphical features of the terranes are compared to those of the neighbouring epicontinental regions (Europe and North Africa) and the Aegean region, representing the Tethyan domain. The detailed ammonoid biostratigraphical subdivision developed in the Alpine region is also correlated with the neighbouring regions. The paleogeographical positions of the terranes are briefly discussed. It is concluded that the crustal fragments carrying the later Alpine-Carpathian terranes were in close connection with the Eurasian continental shelf in the Triassic, while during the Jurassic they belonged to different microcontinents within the western Tethys ocean. © 2000 Elsevier B.V. All rights reserved.},
	year = {2000},
	pages = {173-196}
}

@article{MTMT:1256307,
	title = {Lithospheric structure of the Pannonian basin derived from seismic, gravity and geothermal data},
	url = {https://m2.mtmt.hu/api/publication/1256307},
	author = {Tari, Gábor and Dövényi, Péter and Dunkl, István and Horváth, Ferenc and Lenkey, László and Szafian, P and Toth, T},
	doi = {10.1144/GSL.SP.1999.156.01.12},
	journal-iso = {GEOL SOC SPEC PUBL},
	journal = {GEOLOGICAL SOCIETY SPECIAL PUBLICATIONS},
	volume = {156},
	unique-id = {1256307},
	issn = {0305-8719},
	abstract = {This paper is part of the special publication No.156, The Mediterranean basins: Tertiary extension within the Alpine Orogen. (eds B.Durand, L. Jolivet, F.Horvath and M.Seranne). The structure of the Pannonian basin is the result of distinct modes of Mid-Late Miocene extension exerting a profound effect on the lithospheric configuration, which continues even today. As the first manifestation of extensional collapse, large magnitude, metamorphic core complex style extension took place at the beginning of the Mid-Miocene in certain parts of the basin. Extrapolation of the present-day high heat flow in the basin, corrected for the blanketing effect of the basin fill, indicates a hot and thin lithosphere at the onset of extension. This initial condition, combined with the relatively thick crust inherited from earlier Alpine compressional episodes, appears to be responsible for the core complex type extension at the beginning of the syn-rift period. This type of extension is well documented in the northwestern Pannonian basin. Newly obtained deep reflection seismic and fission-track data integrated with well data from the southeastern part of the basin suggests that it developed in a similar fashion. Shortly after the initial period, the style of syn-rift extension changed to a wide-rift style, covering an area of much larger geographic extent. The associated normal faults revealed by industry reflection seismic data tend to dominate within the upper crust, obscuring pre-existing structures. However, several deep seismic profiles, constrained by gravity and geothermal modeling, image the entire lithosphere beneath the basin. It is the Mid-Miocene synrift extension which is still reflected in the structure of the Pannonian lithosphere, on the scale of the whole basin system. The gradually diminishing extension during the Late Miocene/Pliocene could not advance to the localization of extension into narrow rift zones in the Pannonian region except some deep subbasins such as the Mako/Bekes and Danube basins. These basins are underlain coincidently by anomalously thin crust (22-25 km) and lithosphere (45-60 km). Significant departures (up to 130 mW m -2) from the average present-day surface heat flow for the initiation of two newly defined narrow rift zones (Tisza and Duna) in the Pannonian basin system. However, both of these narrow rifts failed since the final docking of the Eastern Carpathians onto the European foreland excluded any further extension of the back-arc region.},
	year = {1999},
	eissn = {2041-4927},
	pages = {215-250},
	orcid-numbers = {Lenkey, László/0000-0003-4236-4075}
}

@article{MTMT:1635953,
	title = {Petrophysical and sedimentological analyses of Siklós ornamental limestones, S-Hungary},
	url = {https://m2.mtmt.hu/api/publication/1635953},
	author = {Török, Ákos},
	journal-iso = {PERIOD POLYTECH CIV ENG},
	journal = {PERIODICA POLYTECHNICA-CIVIL ENGINEERING},
	volume = {43},
	unique-id = {1635953},
	issn = {0553-6626},
	year = {1999},
	eissn = {1587-3773},
	pages = {187-205},
	orcid-numbers = {Török, Ákos/0000-0002-5394-4510}
}

@article{MTMT:1368457,
	title = {Magyarországi szerkezetföldtani kutatások és ezek legújabb eredményei},
	url = {https://m2.mtmt.hu/api/publication/1368457},
	author = {Fodor, László and Csontos, László},
	journal-iso = {FÖLDTANI KÖZLÖNY},
	journal = {FÖLDTANI KÖZLÖNY},
	volume = {128},
	unique-id = {1368457},
	issn = {0015-542X},
	year = {1998},
	eissn = {2559-902X},
	pages = {123-143},
	orcid-numbers = {Fodor, László/0000-0002-0606-4414}
}

@article{MTMT:21491561,
	title = {Lower Triassic storm-dominated ramp sequence in northern Hungary: An example of evolution from homoclinal through distally steepened ramp to Middle Triassic flat-topped platform.},
	url = {https://m2.mtmt.hu/api/publication/21491561},
	author = {Hips, Kinga},
	doi = {10.1144/GSL.SP.1999.149.01.15},
	journal-iso = {GEOL SOC SPEC PUBL},
	journal = {GEOLOGICAL SOCIETY SPECIAL PUBLICATIONS},
	volume = {149},
	unique-id = {21491561},
	issn = {0305-8719},
	year = {1998},
	eissn = {2041-4927},
	pages = {315-338},
	orcid-numbers = {Hips, Kinga/0000-0003-2315-120X}
}

@article{MTMT:1324065,
	title = {Synsedimentary tectonic events in the Middle Triassic evolution of the SE Transdanubian part of the Tisza Unit},
	url = {https://m2.mtmt.hu/api/publication/1324065},
	author = {Konrád, Gyula},
	journal-iso = {ACTA GEOL HUNG},
	journal = {ACTA GEOLOGICA HUNGARICA: A QUARTERLY OF THE HUNGARIAN ACADEMY OF SCIENCES},
	volume = {41},
	unique-id = {1324065},
	issn = {0236-5278},
	year = {1998},
	pages = {327-341}
}

@article{MTMT:21491562,
	title = {Geodynamic evolution of the central Dinarides.},
	url = {https://m2.mtmt.hu/api/publication/21491562},
	author = {Pamic, J and Gusic, I and Jelaska, V},
	doi = {10.1016/S0040-1951(98)00171-1},
	journal-iso = {TECTONOPHYSICS},
	journal = {TECTONOPHYSICS},
	volume = {297},
	unique-id = {21491562},
	issn = {0040-1951},
	year = {1998},
	eissn = {1879-3266},
	pages = {251-268}
}

@article{MTMT:1635999,
	title = {Controls on development of Mid-Triassic ramps: examples from southern Hungary},
	url = {https://m2.mtmt.hu/api/publication/1635999},
	author = {Török, Ákos},
	doi = {10.1144/GSL.SP.1999.149.01.16},
	journal-iso = {GEOL SOC SPEC PUBL},
	journal = {GEOLOGICAL SOCIETY SPECIAL PUBLICATIONS},
	volume = {149},
	unique-id = {1635999},
	issn = {0305-8719},
	abstract = {During Mid-Triassic time the palaeogeographical-tectonic setting of the northern Tethyan passive margin and epicontinental basins favoured the ramp morphology, as broad flat areas were available for flooding and establishment of carbonate sedimentation. Throughout this time, in what is now southern Hungary, homoclinal ramps developed, which also exhibit some evidence of partial distal steepening. The nearly 1 km thick Anisian-Ladinian Muschelkalk carbonates are grouped into six depositional units. In each ramp unit facies types were identified representing coastal sabkhas, inner ramp peritidal facies, backshoal lagoons, oolite shoals, storm to fair-weather influenced mid-ramps, proximal to distal shell beds and low-energy outer ramps. Mid- and inner ramp carbonates make up the majority of the successions. The deepest outer ramp facies correspond to the peak transgression of a second-order Triassic sea-level rise. In the Hungarian Muschelkalk three major transgressive-regressive sequences were identified. In Germany, Poland and Spain much thinner and slightly coarser Muschelkalk carbonate successions were formed in the same Mid-Triassic interval. The major sediment redistribution processes were related to storms that generated coquinas, and mud flow deposits. Slow, early diagenesis and the predominance of unstable muddy substrate led to the formation of small-scale slumps, slides and plastic deformation. The fauna reflects the prevalence of carbonate mud and temporarily high-stress conditions. A non 'cool water' origin of this ramp is inferred from the presence of evaporites, early dolomization of inner ramp carbonates, the biota and the palaeogeographical setting. The major controlling factors of Mid-Triassic ramps were the gentle antecedent morphology, the subtropical climate, the high production of carbonate mud and the lack of reef-building organisms, as well as the passive margin setting, which resulted in a moderate and relatively uniform subsidence rate over a wide area.},
	year = {1998},
	eissn = {2041-4927},
	pages = {339-367},
	orcid-numbers = {Török, Ákos/0000-0002-5394-4510}
}

@article{MTMT:2224128,
	title = {Bivalve assemblages from the Middle Triassic Muschelkalk of the Mecsek Mts, South Hungary: An overview},
	url = {https://m2.mtmt.hu/api/publication/2224128},
	author = {Szente, István},
	journal-iso = {ACTA GEOL HUNG},
	journal = {ACTA GEOLOGICA HUNGARICA: A QUARTERLY OF THE HUNGARIAN ACADEMY OF SCIENCES},
	volume = {40},
	unique-id = {2224128},
	issn = {0236-5278},
	year = {1997},
	pages = {411-424}
}

@article{MTMT:1635954,
	title = {Dolomitization and karst-related dedolomitzation of Muschelkalk carbonates, in South Hungary},
	url = {https://m2.mtmt.hu/api/publication/1635954},
	author = {Török, Ákos},
	journal-iso = {ACTA GEOL HUNG},
	journal = {ACTA GEOLOGICA HUNGARICA: A QUARTERLY OF THE HUNGARIAN ACADEMY OF SCIENCES},
	volume = {40},
	unique-id = {1635954},
	issn = {0236-5278},
	year = {1997},
	pages = {441-462},
	orcid-numbers = {Török, Ákos/0000-0002-5394-4510}
}

@article{MTMT:1635955,
	title = {Triassic ramp evolution, southern Hungary and its similarities to Germano-type Triassic.},
	url = {https://m2.mtmt.hu/api/publication/1635955},
	author = {Török, Ákos},
	journal-iso = {ACTA GEOL HUNG},
	journal = {ACTA GEOLOGICA HUNGARICA: A QUARTERLY OF THE HUNGARIAN ACADEMY OF SCIENCES},
	volume = {40},
	unique-id = {1635955},
	issn = {0236-5278},
	year = {1997},
	pages = {367-390},
	orcid-numbers = {Török, Ákos/0000-0002-5394-4510}
}

@article{MTMT:1412630,
	title = {Mesozoic igneous suites in Hungary: Implications for genesis and tectonic setting in the northwestern part of Tethys},
	url = {https://m2.mtmt.hu/api/publication/1412630},
	author = {Harangi, Szabolcs and Szabó, Csaba and Józsa, Sándor and Szoldán, Z and Árva-Sós, Erzsébet and Balla, Márta and Kubovics, Imre},
	doi = {10.1080/00206819709465339},
	journal-iso = {INT GEOL REV},
	journal = {INTERNATIONAL GEOLOGY REVIEW},
	volume = {38},
	unique-id = {1412630},
	issn = {0020-6814},
	abstract = {Mesozoic igneous rocks occur in various tectonic units of the Intra-Carpathian Area of Eastern Europe. These rocks were situated several hundred km apart from one another during their formation, and subsequent large lateral displacements resulted in their present positions. They formed during a relatively wide temporal range (Middle Triassic to Late Cretaceous) through different petrogenetic processes associated with the Mesozoic evolution of the northwestern part of Tethys. In the Transdanubian subunit of the Alcapa block, Middle Triassic calc-alkaline, intermediateto-acidic, and potassic rocks occur as pyroclastics, lava flows, and dikes in the Bakony and Buda mountains. The Gemer-Bükk subunit of the Alcapa block comprises two different igneous series: (1) slightly metamorphosed Middle Triassic volcanic rocks of the Eastern Bükk Mountains, which can be divided into an older (Anisian-Early Ladinian) calc-alkaline, intermediateto-acidic volcanic series and a younger (Late Ladinian) alkaline basaltic series; and (2) two series of the Middle Triassic to Middle Jurassic ophiolite complex (Bódva Magmatic Series and Darnó-Szarvaskö Magmatic Series), embedded in a tectonic mélange and in an olistostrome suite along a SW-NE-oriented zone. The Tisza block contains Early Cretaceous alkaline volcanic rocks in the Mecsek-Alföld subunit. Strong temporal and geochemical correlations have been observed between the Middle Triassic volcanic rocks of the Bakony and Buda mountains and the Southern Alps, and those of the Eastern Bükk Mountains and the Outer Dinarides. We propose that all these rocks were formed during the same extension-related volcanic activity along the Southern Alps-Bakony and Buda mountains-Eastern Bükk Mountains-Dinarides region. The Middle Triassic-Middle Jurassic ultramafic-mafic igneous rocks of the Gemer-Bükk subunit can be correlated with the ophiolites of the Inner Dinarides. Geochemistry of the mafic rocks is consistent with an origin from an N-MORB and E-MORB source mantle. The Middle to Late Triassic ultramafic and mafic rocks of the Bódva and Darnó-Szarvaskö series could have originated along the mid-oceanic ridge system of the northwestern segment of the Vardar ocean (Meliaticum). The Middle Jurassic igneous rocks of the Darnó-Szarvaskö series could have corresponded to the opening of a backarc basin. Early Cretaceous alkaline volcanic rocks of the Mecsek-Alföld zone in the Tisza block formed as a result of continental rifting along the southern margin of the European plate. Two volcanic series - a mafic and a sodic group - were generated from an OIB-like asthenospheric mantle. Separation of the Tisza block from the European plate occurred contemporaneously with volcanic activity during the late Early Cretaceous.},
	keywords = {Hungary; tectonic setting; Tethys; igneous rock; Mesozoic; petrogenesis},
	year = {1996},
	eissn = {1938-2839},
	pages = {336-360},
	orcid-numbers = {Harangi, Szabolcs/0000-0003-2372-4581; Szabó, Csaba/0000-0002-1580-6344; Józsa, Sándor/0000-0001-8219-0044}
}

@article{MTMT:152253,
	title = {Stratigraphical and facies evaluation of the Lower Triassic formations in the Aggtelek-Rudabánya Mountains, NE Hungary},
	url = {https://m2.mtmt.hu/api/publication/152253},
	author = {Hips, Kinga},
	journal-iso = {ACTA GEOL HUNG},
	journal = {ACTA GEOLOGICA HUNGARICA: A QUARTERLY OF THE HUNGARIAN ACADEMY OF SCIENCES},
	volume = {39},
	unique-id = {152253},
	issn = {0236-5278},
	year = {1996},
	pages = {369-411},
	orcid-numbers = {Hips, Kinga/0000-0003-2315-120X}
}