@article{MTMT:3091740,
	title = {Processes and controlling factors of polygenetic dolomite formation in the Transdanubian Range, Hungary: a synopsis},
	url = {https://m2.mtmt.hu/api/publication/3091740},
	author = {Haas, János and Hips, Kinga and Budai, Tamás and Győri, Orsolya and Lukoczki, Georgina and Kele, Sándor and Demény, Attila and Poros, Zsófia},
	doi = {10.1007/s00531-016-1347-7},
	journal-iso = {INT J EARTH SCI},
	journal = {INTERNATIONAL JOURNAL OF EARTH SCIENCES},
	volume = {106},
	unique-id = {3091740},
	issn = {1437-3254},
	year = {2017},
	eissn = {1437-3262},
	pages = {991-1021},
	orcid-numbers = {Haas, János/0000-0003-0929-8889; Hips, Kinga/0000-0003-2315-120X; Győri, Orsolya/0000-0002-3646-9113; Lukoczki, Georgina/0000-0002-0661-0198; Kele, Sándor/0000-0002-8607-7636; Demény, Attila/0000-0003-0522-9018}
}

@article{MTMT:2922731,
	title = {A multi-system geochronology in the Ad-3 borehole, Pannonian Basin (Hungary) with implications for dating volcanic rocks by low-temperature thermochronology and for interpretation of (U-Th)/He data},
	url = {https://m2.mtmt.hu/api/publication/2922731},
	author = {Danišík, M and Fodor, László and Dunkl, István and Gerdes, A and Csizmeg, János and Hámorné, Vidó Mária and Evans, NJ},
	doi = {10.1111/ter.12155},
	journal-iso = {TERRA NOVA},
	journal = {TERRA NOVA},
	volume = {27},
	unique-id = {2922731},
	issn = {0954-4879},
	year = {2015},
	eissn = {1365-3121},
	pages = {258-269}
}

@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}
}

@article{MTMT:152141,
	title = {Facies and diagenetic evaluation of the Permian-Triassic boundary interval and basal Triassic carbonates: shallow and deep ramp sections, Hungary.},
	url = {https://m2.mtmt.hu/api/publication/152141},
	author = {Hips, Kinga and Haas, János},
	doi = {10.1007/s10347-009-0182-8},
	journal-iso = {FACIES},
	journal = {FACIES},
	volume = {55},
	unique-id = {152141},
	issn = {0172-9179},
	year = {2009},
	eissn = {1612-4820},
	pages = {421-442},
	orcid-numbers = {Hips, Kinga/0000-0003-2315-120X; Haas, János/0000-0003-0929-8889}
}

@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:1019032,
	title = {Triassic sequence stratigraphy of the Transdanubian Range (Hungary)},
	url = {https://m2.mtmt.hu/api/publication/1019032},
	author = {Haas, János and Budai, Tamás},
	journal-iso = {GEOL CARPATH},
	journal = {GEOLOGICA CARPATHICA},
	volume = {50},
	unique-id = {1019032},
	issn = {1335-0552},
	abstract = {On the basis of surface exposures and core sections, a comprehensive sequence analysis of the Triassic series was carried out in the Transdanubian Range. For recognition of the sequences as well as their boundaries, the regional subaerial exposure horizons, the maximum flooding intervals, the transgressive-regressive trends, the platform progradations and backsteppings, as well as signals of the higher order accommodation changes were primarily considered. Detailed analyses were accomplished in six selected sub-regions. On the basis of the results of these analyses, a composite sequence chart was compiled. The Triassic history of the Transdanubian Range can be subdivided into four stages. Within the first stage (Induan to Middle Anisian) which can be characterized by a ramp setting, five sequences have been recognized. The second stage (Middle Anisian-Ladinian) is mainly controlled by the Neotethys rifting and can be subdivided into three sequences. Infilling of the previously formed basins took place during the third stage (Carnian), consisting of three sequences. The fourth stage (latest Carnian to Rhaetian) reflects the passive margin evolution of the Neotethys. However, a new rifting (Ligurian-Penninic) began in the Late Norian and also influenced the evolution of the Transdanubian Range. Four sequences were recognized in this final evolutionary stage. About 50 % of the recognized sequence boundaries could be correlated with those reported from the Southern and Northern Alps, from the German Basin, and from Western Canada.},
	year = {1999},
	eissn = {1336-8052},
	pages = {459-475},
	orcid-numbers = {Haas, János/0000-0003-0929-8889}
}

@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: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: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}
}