@{MTMT:34342977,
	title = {Paleozoikum},
	url = {https://m2.mtmt.hu/api/publication/34342977},
	author = {Halász, Amadé and Haranginé Lukács, Réka and Koroknai, B and Less, György and Raucsikné Varga, Andrea Beáta and Lelkesné Felvári, Gy and Józsa, Sándor and Kovács, Sándor and Király, Edit and Benkó, Zsolt and Majoros, Gy and Pentelényi, L and Szederkényi, T and Rálischné Felgenhauer, E and Pelikán, P and Szemerédi, Máté and Konrád, Gy and Barabásné Stuhl, Á and Pál-Molnár, E},
	booktitle = {Magyarország litosztratigráfiai egységeinek leírása I.},
	unique-id = {34342977},
	year = {2023},
	pages = {43-112},
	orcid-numbers = {Halász, Amadé/0000-0003-4582-8883; Haranginé Lukács, Réka/0000-0002-2338-4209; Raucsikné Varga, Andrea Beáta/0000-0002-8673-1482; Józsa, Sándor/0000-0001-8219-0044; Szemerédi, Máté/0000-0002-7432-8418}
}

@article{MTMT:2725896,
	title = {EVIDENCE FOR LADINIAN (MIDDLE TRIASSIC) PLATFORM PROGRADATION IN THE GYULAKESZI AREA, TAPOLCA BASIN, WESTERN HUNGARY: MICROFACIES ANALYSIS AND BIOSTRATIGRAPHY},
	url = {https://m2.mtmt.hu/api/publication/2725896},
	author = {Nagy, ZR and Djeric, N and Kovács, Sándor and Oravecz-Scheffer, A and Velledits, Felicitász and Piros, Olga and Csillag, Gábor},
	doi = {10.13130/2039-4942/6058},
	journal-iso = {RIV IT PALEON STRATIG},
	journal = {RIVISTA ITALIANA DI PALEONTOLOGIA E STRATIGRAFIA},
	volume = {120},
	unique-id = {2725896},
	issn = {0035-6883},
	abstract = {A shallowing-upward carbonate sequence was studied from the outcrop at Gyulakeszi, Tapolca Basin (western Hungary), and it is interpreted as a Middle Triassic (Curionii or younger) platform progradation. Two lithostratigraphic units are distinguished. Microfacies analysis and micropaleontological investigation conducted on the red nodular, cherry limestone (Vaszoly and Buchenstein formations) suggest that the lower unit was deposited during the Reitzi and the Secedensis ammonoid zones. The overlying white platform limestone (upper unit) is typical of a prograding platform and includes gravity-driven deposits at the base followed by periplatform facies deposited in shallow marine warm waters around the fair-weather wave base. The section at Gyulakeszi was unaffected by fabric-destructive dolomitization, which is uncharacteristic of similar platform facies in the Balaton Highland. Isopachous and radiaxial fibrous calcite cement found in the grainstone and boundstone facies are indicative of early lithification and diagenesis in the marine phreatic zone. "Evinospongiae"-type cement is described for the first time from the Balaton Highland and it is similar to the outer platform cements published previously from the Alps (Italy and Austria). The progradation could have advanced over the pelagic limestones as early as the Curionii zone, which is an undocumented event in the Veszprem Plateau. Similar event, however, is well known from the Western Dolomites, where aggradation was followed by intense progradation during the Gredleri and Archelaus ammonoid zones. The length of this progradation event at Gyulakeszi, however, is ambiguous since proven Ladinian (Longobardian) rocks are not exposed in the study area and were not penetrated by boreholes in the Tapolca Basin.},
	year = {2014},
	eissn = {2039-4942},
	pages = {165-181}
}

@book{MTMT:1437346,
	title = {Variscan and Alpine terranes of the Circum-Pannonian region},
	url = {https://m2.mtmt.hu/api/publication/1437346},
	isbn = {9788097160999},
	editor = {Vozár, J and Ebner, F and Vozarová, A and Haas, János and Kovács, Sándor and Sudar, M and Bielik, M and Péró, Csaba},
	publisher = {Slovenská akadémia vied},
	unique-id = {1437346},
	year = {2014},
	orcid-numbers = {Haas, János/0000-0003-0929-8889}
}

@article{MTMT:2063788,
	title = {Revised Middle and Late Triassic radiolarian ages for ophiolite mélanges: implications for the geodynamic evolution of the northern part of the early Mesozoic Neotethyan subbasins},
	url = {https://m2.mtmt.hu/api/publication/2063788},
	author = {Ozsvárt, Péter and Kovács, Sándor},
	doi = {10.2113/gssgfbull.183.4.273},
	journal-iso = {B SOC GEOL FR},
	journal = {BULLETIN DE LA SOCIETE GEOLOGIQUE DE FRANCE / EARTH SCIENCES BULLETIN},
	volume = {183},
	unique-id = {2063788},
	issn = {0037-9409},
	abstract = {The study is based on the radiolarian assemblages of five radiolarite outcrops and two boreholes from the Darnó and Szarvaskő Complex, Hungary, and three radiolarite sections from the western Vardar Ophiolitic Unit in Serbia. These investigated sections belong to a Mesozoic volcano-sedimentary mélange belt that can be followed from the Hellenides, through the Dinarides to the western Carpathians. Samples from radiolarite localities in the Darnó and Szarvaskő Complex contain a mixture of Middle Triassic (Illyrian to Longobardian) and Upper Triassic (Carnian) fairly poorly preserved radiolarian assemblages. Radiolarite samples from the western Vardar Ophiolitic Unit (Gostilje, Krš Gradac and Bukovi) yielded poorly preserved Upper Triassic (Carnian-?Norian) radiolarians. Co-occurrences of Middle and Upper Triassic radiolarian specimens in Darnó and Szarvaskő Complex suggest resedimentation during the Carnian or later. One new radiolarian species (Baumgartneria szarvaskoensis n. sp.) is described herein from the Darnó and Szarvaskő Complex.},
	year = {2012},
	eissn = {1777-5817},
	pages = {273-286}
}

@article{MTMT:1461439,
	title = {New radiolarian biostratigraphic age constraints on Middle Triassic basalts and radiolarites from the inner Hellenides (Northern Pindos and Othrys Mountains, Northern Greece) and their implications for the geodynamic evolution of the early Mesozoic Neotethys},
	url = {https://m2.mtmt.hu/api/publication/1461439},
	author = {Ozsvárt, Péter and Dosztály, L and Migiros, G and Tselepidis, V and Kovács, Sándor},
	doi = {10.1007/s00531-010-0628-9},
	journal-iso = {INT J EARTH SCI},
	journal = {INTERNATIONAL JOURNAL OF EARTH SCIENCES},
	volume = {101},
	unique-id = {1461439},
	issn = {1437-3254},
	year = {2012},
	eissn = {1437-3262},
	pages = {1487-1501}
}

@article{MTMT:1827129,
	title = {Jurassic evolution of the tectonostratigraphic units in the Circum-Pannonian region.},
	url = {https://m2.mtmt.hu/api/publication/1827129},
	author = {Haas, János and Kovács, Sándor and Gawlick, H-J and Grădinaru, E and Karamata, S and Sudar, M and Péró, Csaba and Mello, J and Polák, M and Ogorelec, B and Buser, S},
	journal-iso = {JAHRB GEOL BUNDESANST},
	journal = {JAHRBUCH DER GEOLOGISCHEN BUNDESANSTALT},
	volume = {151},
	unique-id = {1827129},
	issn = {0016-7800},
	year = {2011},
	pages = {281­-354},
	orcid-numbers = {Haas, János/0000-0003-0929-8889}
}

@article{MTMT:1827113,
	title = {Triassic evolution of the tectonostratigraphic units in the Circum-Pannonian region},
	url = {https://m2.mtmt.hu/api/publication/1827113},
	author = {Kovács, Sándor and Sudar, M and Grădinaru, E and Karamata, S and Gawlick, H-J and Haas, János and Péró, Csaba and Gaetani, M and Mello, J and Polák, M and Aljinicic, D and Ogorelec, B and Kollar-Jurkovsek, T and Jurkovsek, B and Buser, S},
	journal-iso = {JAHRB GEOL BUNDESANST},
	journal = {JAHRBUCH DER GEOLOGISCHEN BUNDESANSTALT},
	volume = {151},
	unique-id = {1827113},
	issn = {0016-7800},
	year = {2011},
	pages = {199-280},
	orcid-numbers = {Haas, János/0000-0003-0929-8889}
}

@article{MTMT:1683406,
	title = {The oldest Triassic platform margin reef from the Alpine–Carpathian region (Aggtelek, NE Hungary): Platform evolution, reefal biota and biostratigraphic framework},
	url = {https://m2.mtmt.hu/api/publication/1683406},
	author = {Velledits, Felicitász and Péró, Csaba and Blau, J and Senowbari-Daryan, B and Kovács, Sándor and Piros, Olga and Pocsai, T and Szügyi-Simon, H and Dumitrică, P and Pálfy, József},
	doi = {10.13130/2039-4942/5973},
	journal-iso = {RIV IT PALEON STRATIG},
	journal = {RIVISTA ITALIANA DI PALEONTOLOGIA E STRATIGRAFIA},
	volume = {117},
	unique-id = {1683406},
	issn = {0035-6883},
	year = {2011},
	eissn = {2039-4942},
	pages = {221-268},
	orcid-numbers = {Pálfy, József/0000-0001-9686-1849}
}

@article{MTMT:1438847,
	title = {Displaced South Alpine and Dinaridic elements in the Mid-Hungarian Zone},
	url = {https://m2.mtmt.hu/api/publication/1438847},
	author = {Haas, János and Kovács, Sándor and Karamata, S and Sudar, M},
	journal-iso = {BULL ACAD SERBE SCI ARTS CL SCI MATH NAT SCI NAT},
	journal = {BULLETIN SCIENCES NATURELLES ACADEMIE SERBE DES SCIENCES ET DES ARTS CLASSE DES SCIENCES MATHEMATIQUES ET NATURELLES},
	volume = {46},
	unique-id = {1438847},
	issn = {0352-5740},
	year = {2010},
	pages = {81-103},
	orcid-numbers = {Haas, János/0000-0003-0929-8889}
}

@inbook{MTMT:1437350,
	title = {Jurassic environments in the Circum-Pannonian region},
	url = {https://m2.mtmt.hu/api/publication/1437350},
	author = {Haas, János and Kovács, Sándor and Karamata, S and Sudar, M and Gawlick, H-J and Grădinaru, E and Mello, J and Polák, M and Péró, Csaba and Ogorelec, B and Buser, S},
	booktitle = {Variscan and Alpine terranes of the Circum-Pannonian Region},
	unique-id = {1437350},
	year = {2010},
	pages = {157-202},
	orcid-numbers = {Haas, János/0000-0003-0929-8889}
}