@article{MTMT:2474971,
	title = {Geochemistry of the Görcsöny Ridge amphibolites (Tisza Unit, SW Hungary) and its geodynamic consequences},
	url = {https://m2.mtmt.hu/api/publication/2474971},
	author = {M. Tóth, Tivadar},
	doi = {10.4154/GC.2014.02},
	journal-iso = {GEOL CROAT},
	journal = {GEOLOGIA CROATICA},
	volume = {67},
	unique-id = {2474971},
	issn = {1330-030X},
	abstract = {in press},
	year = {2014},
	eissn = {1333-4875},
	pages = {17-32},
	orcid-numbers = {M. Tóth, Tivadar/0000-0003-1012-1095}
}

@article{MTMT:2808607,
	title = {Petrochemistry of Variscan granitoids of Central Europe: Correlation of Variscan granitoids of Tisia and Pelsonian Terranes with granitoids of Moldanubicum, Western Carpathian and Southern Alps. A review: part I.},
	url = {https://m2.mtmt.hu/api/publication/2808607},
	author = {Buda, György and Koller, F and Ulrych, J},
	doi = {10.1556/AGeol.47.2004.2-3.3},
	journal-iso = {ACTA GEOL HUNG},
	journal = {ACTA GEOLOGICA HUNGARICA: A QUARTERLY OF THE HUNGARIAN ACADEMY OF SCIENCES},
	volume = {47},
	unique-id = {2808607},
	issn = {0236-5278},
	year = {2004},
	pages = {117-138}
}

@article{MTMT:2808782,
	title = {Zircon typology, geochronology and whole rock Sr-Nd isotope systematics of the Mecsek Mountain granitoids in the Tisia Terrane (Hungary)},
	url = {https://m2.mtmt.hu/api/publication/2808782},
	author = {Klötzli, U and Buda, György and Skiöld, T},
	doi = {10.1007/s00710-003-0026-0},
	journal-iso = {MINER PETROL},
	journal = {MINERALOGY AND PETROLOGY},
	volume = {81},
	unique-id = {2808782},
	issn = {0930-0708},
	year = {2004},
	eissn = {1438-1168},
	pages = {113-134}
}

@article{MTMT:1004506,
	title = {Eclogite and garnet amphibolite pebbles from Miocene conglomerates (Pannonian Basin, Hungary): Implications for the Variscan metamorphic evolution of the Tisza Megaunit},
	url = {https://m2.mtmt.hu/api/publication/1004506},
	author = {Horváth, Péter and Kovacs, G and Szakmány, György},
	journal-iso = {GEOL CARPATH},
	journal = {GEOLOGICA CARPATHICA},
	volume = {54},
	unique-id = {1004506},
	issn = {1335-0552},
	year = {2003},
	eissn = {1336-8052},
	pages = {355-366},
	orcid-numbers = {Szakmány, György/0000-0002-9557-2030}
}

@article{MTMT:1302285,
	title = {Petrology and geochemistry of Upper Carboniferous siliciclastic rocks (Téseny Sandstone Formation) from the Slavonian-Drava Unit (Tisza Megaunit, S Hungary) - summarized results},
	url = {https://m2.mtmt.hu/api/publication/1302285},
	author = {Raucsikné Varga, Andrea Beáta and Szakmány, György and Józsa, Sándor and Máthé, Zoltán},
	doi = {10.1556/AGeol.46.2003.1.7},
	journal-iso = {ACTA GEOL HUNG},
	journal = {ACTA GEOLOGICA HUNGARICA: A QUARTERLY OF THE HUNGARIAN ACADEMY OF SCIENCES},
	volume = {46},
	unique-id = {1302285},
	issn = {0236-5278},
	year = {2003},
	pages = {95-113},
	orcid-numbers = {Raucsikné Varga, Andrea Beáta/0000-0002-8673-1482; Szakmány, György/0000-0002-9557-2030; Józsa, Sándor/0000-0001-8219-0044}
}

@article{MTMT:1155192,
	title = {The Tisza megatectonic unit in the light of paleomagnetic data},
	url = {https://m2.mtmt.hu/api/publication/1155192},
	author = {Márton Péterné Szalay, Emőke},
	journal-iso = {ACTA GEOL HUNG},
	journal = {ACTA GEOLOGICA HUNGARICA: A QUARTERLY OF THE HUNGARIAN ACADEMY OF SCIENCES},
	volume = {43},
	unique-id = {1155192},
	issn = {0236-5278},
	year = {2000},
	pages = {329-343},
	orcid-numbers = {Márton Péterné Szalay, Emőke/0000-0002-2135-8867}
}

@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: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:1659720,
	title = {Rb-Sr isotopic studies on granodioritic rocks from the Mecsek Mountains,Hungary.},
	url = {https://m2.mtmt.hu/api/publication/1659720},
	author = {Sudár Sándorné Svingor, Éva and Kovách, Ádám},
	journal-iso = {ACTA GEOL HUNG},
	journal = {ACTA GEOLOGICA HUNGARICA: A QUARTERLY OF THE HUNGARIAN ACADEMY OF SCIENCES},
	volume = {24},
	unique-id = {1659720},
	issn = {0236-5278},
	year = {1981},
	pages = {295}
}