@article{MTMT: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},
	title = {Processes and controlling factors of polygenetic dolomite formation in the Transdanubian Range, Hungary: a synopsis},
	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}
}

@article{MTMT:2922731,
	author = {Danišík, M and Fodor, László and Dunkl, I and Gerdes, A and Csizmeg, János and Hámorné, Vidó Mária and Evans, NJ},
	doi = {10.1111/ter.12155},
	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},
	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,
	author = {Haas, János and Budai, Tamás and Raucsik, Béla},
	doi = {10.1016/j.palaeo.2012.06.031},
	title = {Climatic controls on sedimentary environments in the Triassic of the Transdanubian Range (Western Hungary)},
	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,
	author = {Hips, Kinga and Haas, János},
	doi = {10.1007/s10347-009-0182-8},
	title = {Facies and diagenetic evaluation of the Permian-Triassic boundary interval and basal Triassic carbonates: shallow and deep ramp sections, Hungary.},
	journal-iso = {FACIES},
	journal = {FACIES},
	volume = {55},
	unique-id = {152141},
	issn = {0172-9179},
	year = {2009},
	pages = {421-442},
	orcid-numbers = {Hips, Kinga/0000-0003-2315-120X; Haas, János/0000-0003-0929-8889}
}

@article{MTMT:1236932,
	author = {Csontos, L and Vörös, Attila},
	doi = {10.1016/j.palaeo.2004.02.033},
	title = {Mesozoic plate tectonic reconstruction of the carpathian region},
	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,
	author = {Haas, János and Budai, Tamás},
	title = {Triassic sequence stratigraphy of the Transdanubian Range (Hungary)},
	journal-iso = {GEOL CARPATH},
	journal = {GEOLOGICA CARPATHICA},
	volume = {50},
	unique-id = {1019032},
	issn = {1335-0552},
	year = {1999},
	pages = {459-475},
	orcid-numbers = {Haas, János/0000-0003-0929-8889}
}

@article{MTMT:1019016,
	author = {Haas, János and Kovács, Sándor and L, Krystyn and R, Lein},
	doi = {10.1016/0040-1951(94)00157-5},
	title = {Significance of Late Permian-Triassic facies zones in terrane reconstructions in the Alpine North Pannonian domain},
	journal-iso = {TECTONOPHYSICS},
	journal = {TECTONOPHYSICS},
	volume = {242},
	unique-id = {1019016},
	issn = {0040-1951},
	year = {1995},
	pages = {19-40},
	orcid-numbers = {Haas, János/0000-0003-0929-8889}
}

@article{MTMT:1255443,
	author = {CSONTOS, L and Nagymarosy, András (1949-2016) and Horváth, Ferenc and KOVAC, M},
	doi = {10.1016/0040-1951(92)90346-8},
	title = {TERTIARY EVOLUTION OF THE INTRA-CARPATHIAN AREA - A MODEL},
	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},
	pages = {221-241}
}