@article{MTMT:1025551,
	title = {Triassic sequence stratigraphy of the Balaton Highland, Hungary},
	url = {https://m2.mtmt.hu/api/publication/1025551},
	author = {Budai, Tamás and Haas, János},
	journal-iso = {ACTA GEOL HUNG},
	journal = {ACTA GEOLOGICA HUNGARICA: A QUARTERLY OF THE HUNGARIAN ACADEMY OF SCIENCES},
	volume = {40},
	unique-id = {1025551},
	issn = {0236-5278},
	year = {1997},
	pages = {307-335},
	orcid-numbers = {Haas, János/0000-0003-0929-8889}
}

@article{MTMT:1324007,
	title = {Crinoids from the Muschelkalk of the Mecsek Mountains and their stratigraphic significance},
	url = {https://m2.mtmt.hu/api/publication/1324007},
	author = {Hagdorn, H and Konrád, Gyula and Török, Ákos},
	journal-iso = {ACTA GEOL HUNG},
	journal = {ACTA GEOLOGICA HUNGARICA: A QUARTERLY OF THE HUNGARIAN ACADEMY OF SCIENCES},
	volume = {40},
	unique-id = {1324007},
	issn = {0236-5278},
	year = {1997},
	pages = {391-410},
	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:1467974,
	title = {Ostracods and charophytes from the Triassic Kantavár Formation, Mecsek Mts, Hungary},
	url = {https://m2.mtmt.hu/api/publication/1467974},
	author = {Monostori, Miklós},
	journal-iso = {ACTA GEOL HUNG},
	journal = {ACTA GEOLOGICA HUNGARICA: A QUARTERLY OF THE HUNGARIAN ACADEMY OF SCIENCES},
	volume = {39},
	unique-id = {1467974},
	issn = {0236-5278},
	year = {1996},
	pages = {311-317}
}

@article{MTMT:1019328,
	title = {Early Alpine shelf evolution in the Hungarian segments of the Tethys margin},
	url = {https://m2.mtmt.hu/api/publication/1019328},
	author = {Haas, János and Kovács, Sándor and Török, Ákos},
	journal-iso = {ACTA GEOL HUNG},
	journal = {ACTA GEOLOGICA HUNGARICA: A QUARTERLY OF THE HUNGARIAN ACADEMY OF SCIENCES},
	volume = {38},
	unique-id = {1019328},
	issn = {0236-5278},
	year = {1995},
	pages = {95-110},
	orcid-numbers = {Haas, János/0000-0003-0929-8889; Török, Ákos/0000-0002-5394-4510}
}

@article{MTMT:1019016,
	title = {Significance of Late Permian-Triassic facies zones in terrane reconstructions in the Alpine-North Pannonian domain},
	url = {https://m2.mtmt.hu/api/publication/1019016},
	author = {Haas, János and Kovács, Sándor and Krystyn, L and Lein, R},
	doi = {10.1016/0040-1951(94)00157-5},
	journal-iso = {TECTONOPHYSICS},
	journal = {TECTONOPHYSICS},
	volume = {242},
	unique-id = {1019016},
	issn = {0040-1951},
	abstract = {The present-day setting of the tectonic units (terranes) making up the pre-Neogene basement of the Pannonian Basin and the West Carpathians is the result of large-scale displacements during the Alpine collisional phases. To explain this setting, based on various concepts, a number of models have been proposed in the last decade. Most of them agree in an eastward escape of the ''North Pannonian terrane'' from the Alpine domain towards the Pannonian during the Palaeogene-Early Miocene period.
		
		In the present paper a reconstruction of the pre-escape setting of the displaced terranes is presented based on facies zones in selected time-slices from the Late Permian to the Late Triassic. According to our reconstruction the Inner West Carpathian units were located east of the Austroalpine units forming the northern shelf of the ''Euhallstatt''-Meliatic basin of the Vardar oceanic branch. The Drauzug should have been located in a position much more external than its present-day setting. The Transdanubian Range was situated in the northern neighbourhood of the Southern Alps, whereas the Bukk may have been located adjacent to the NW Dinarides. The Mid-Transdanubian zone is a major shear-zone containing elements of the Julian Alps and Sava folds nappe system and the Inner Dinaric ophiolitic melange.
		
		Although the nappe-tectonism may have played an important role in the structural evolution of the ''North Pannonian terrane'', this mechanism alone can hardly produce hundreds of kilometres of facies offset on the opposite sides of strike-slip zones.},
	year = {1995},
	eissn = {1879-3266},
	pages = {19-40},
	orcid-numbers = {Haas, János/0000-0003-0929-8889}
}

@article{MTMT:1019017,
	title = {Upper Permian-Triassic facies zones in the Transdanubian Range},
	url = {https://m2.mtmt.hu/api/publication/1019017},
	author = {Haas, János and Budai, Tamás},
	journal-iso = {RIV IT PALEON STRATIG},
	journal = {RIVISTA ITALIANA DI PALEONTOLOGIA E STRATIGRAFIA},
	volume = {101},
	unique-id = {1019017},
	issn = {0035-6883},
	year = {1995},
	eissn = {2039-4942},
	pages = {249-266},
	orcid-numbers = {Haas, János/0000-0003-0929-8889}
}

@article{MTMT:1025533,
	title = {Triassic facies types, evolution and paleogeographic relations of the Tisza Megaunit},
	url = {https://m2.mtmt.hu/api/publication/1025533},
	author = {M, Bleahu and Mantea, G and Bordea, S and Panin, S and Stefanescu, M and Sikic, K and Haas, János and Kovács, Sándor and Péró, Csaba and Bérczi-Makk, A and Konrád, Gyula and Nagy, E and Rálisch-Felgenhauer, E and Török, Ákos},
	journal-iso = {ACTA GEOL HUNG},
	journal = {ACTA GEOLOGICA HUNGARICA: A QUARTERLY OF THE HUNGARIAN ACADEMY OF SCIENCES},
	volume = {37},
	unique-id = {1025533},
	issn = {0236-5278},
	year = {1994},
	pages = {187-234},
	orcid-numbers = {Haas, János/0000-0003-0929-8889; Török, Ákos/0000-0002-5394-4510}
}

@article{MTMT:1397859,
	title = {Evolution of Middle Triassic shallow marine carbonates in the Balaton Highland (Hungary)},
	url = {https://m2.mtmt.hu/api/publication/1397859},
	author = {Budai, Tamás and LELKES, GY and Piros, Olga},
	journal-iso = {ACTA GEOL HUNG},
	journal = {ACTA GEOLOGICA HUNGARICA: A QUARTERLY OF THE HUNGARIAN ACADEMY OF SCIENCES},
	volume = {36},
	unique-id = {1397859},
	issn = {0236-5278},
	year = {1993},
	pages = {145-165}
}

@article{MTMT:1255443,
	title = {TERTIARY EVOLUTION OF THE INTRA-CARPATHIAN AREA - A MODEL},
	url = {https://m2.mtmt.hu/api/publication/1255443},
	author = {CSONTOS, L and Nagymarosy, András and Horváth, Ferenc and KOVAC, M},
	doi = {10.1016/0040-1951(92)90346-8},
	journal-iso = {TECTONOPHYSICS},
	journal = {TECTONOPHYSICS},
	volume = {208},
	unique-id = {1255443},
	issn = {0040-1951},
	abstract = {The Outer Carpathian flysch nappes encircle an Intra-Carpathian domain
		which can be divided into two megatectonic units (North Pannonian and
		Tisza) mostly on the basis of contrasting Mesozoic and Palaeogene
		facies development. We see two major kinematic problems to be solved:
		(1) The present distribution of the Mesozoic and Palaeogene facies is
		mosaic-like, and some belts form exotic bodies within realms of
		Austroalpine affinity. (2) Late Eocene palinspastic reconstruction of
		the Outer Carpathian flysch nappes suggest, that the entire
		Intra-Carpathian area must have been located several hundreds of
		kilometres to the south and to the west of its present position.
		Neogene extension can account for shortening in the external Carpathian
		nappes, but is unable to explain Mesozoic facies anomalies and offsets
		of Palaeogene formations. We suggest that evolution of the
		Intra-Carpathian area involved first Late Palaeogene-Early Miocene
		juxtaposition of the North-Pannonian and Tisza megatectonic units,
		accompanied by the closure of the external Carpathian flysch troughs;
		thereafter extension of this amalgamated unit occurred, which was
		compensated by thrusting of flysch nappes onto the European foreland
		and formation of molasse foredeeps.
		Eastward escape of the North-Pannonian unit from the Alpine collisional
		belt involved left lateral shear along the Pieniny Klippen belt and
		right lateral shear along the Mid-Hungarian zone. Parts of the Late
		Palaeogene basin and an Early Miocene volcanic edifice were dissected,
		offset and elongated by several 100 kms. The driving mechanism of the
		eastward escape of the Intra-Carpathian area can be related to the
		collision of Apulia and Europe and the subduction of the external
		Carpathian crust under the Pannonian units. The escape ceased gradually
		in the Early Miocene, when oblique collision between the
		North-Pannonian unit and European continent occurred.
		Neogene extension of the Pannonian region was an areal deformation. The
		extension at locally variable rate resulted in the break-up of the
		heterogenous floor of the Neogene basin.
		The driving mechanism of basin extension and contemporaneous
		compressional deformation of the external Carpathians is thought to be
		related to ongoing subduction, involving the marginal part of the
		attenuated European continental crust. Tectonic activity in the
		Carpathians and basin subsidence and volcanism shifted in time and in
		unison from the west toward the east-southeast.},
	year = {1992},
	eissn = {1879-3266},
	pages = {221-241}
}

@article{MTMT:1043702,
	title = {Comparison of Alpine and Germano-type Middle Triassic brachiopod faunas from Hungary, with remarks on Coenothyris vulgaris (Schlotheim 1820)},
	url = {https://m2.mtmt.hu/api/publication/1043702},
	author = {Pálfy, József and Török, Ákos},
	journal-iso = {ANN UNIV SCI BP R EÖTVÖS NOM SECT GEOL},
	journal = {ANNALES UNIVERSITATIS SCIENTIARUM BUDAPESTINENSIS DE ROLANDO EÖTVÖS NOMINATAE - SECTIO GEOLOGICA},
	volume = {29},
	unique-id = {1043702},
	issn = {0365-0634},
	year = {1992},
	pages = {303-323},
	orcid-numbers = {Pálfy, József/0000-0001-9686-1849; Török, Ákos/0000-0002-5394-4510}
}

@inbook{MTMT:1019374,
	title = {The Tisza Superunit was originally part of the North Tethyan (European) margin},
	url = {https://m2.mtmt.hu/api/publication/1019374},
	author = {Kovács, Sándor and Császár, Géza and Galácz, András and Haas, János and Nagy, E and Vörös, Attila},
	booktitle = {Evolution of the Northern margin of Tethys: The results of IGCP Project 198},
	unique-id = {1019374},
	year = {1989},
	pages = {82-100},
	orcid-numbers = {Haas, János/0000-0003-0929-8889}
}

@article{MTMT:1834166,
	title = {Tectonic units of Hungary: Their boundaries and stratigraphy (A bibliographic guide).},
	url = {https://m2.mtmt.hu/api/publication/1834166},
	author = {Kázmér, Miklós},
	journal-iso = {ANN UNIV SCI BP R EÖTVÖS NOM SECT GEOL},
	journal = {ANNALES UNIVERSITATIS SCIENTIARUM BUDAPESTINENSIS DE ROLANDO EÖTVÖS NOMINATAE - SECTIO GEOLOGICA},
	volume = {26},
	unique-id = {1834166},
	issn = {0365-0634},
	year = {1986},
	pages = {45-120},
	orcid-numbers = {Kázmér, Miklós/0000-0003-1092-1316}
}