@article{MTMT:30658244,
	title = {Provenance and Variscan low-grade regional metamorphism recorded in slates from the basement of the (SW Hungary)},
	url = {https://m2.mtmt.hu/api/publication/30658244},
	author = {Mészáros, Előd and Raucsikné Varga, Andrea Beáta and Raucsik, Béla and Benkó, Zsolt and Heincz, Adrián László and Hauzenberger, CA},
	doi = {10.1007/s00531-019-01720-y},
	journal-iso = {INT J EARTH SCI},
	journal = {INTERNATIONAL JOURNAL OF EARTH SCIENCES},
	volume = {108},
	unique-id = {30658244},
	issn = {1437-3254},
	year = {2019},
	eissn = {1437-3262},
	pages = {1571-1593},
	orcid-numbers = {Mészáros, Előd/0000-0002-5846-9034; Raucsikné Varga, Andrea Beáta/0000-0002-8673-1482; Raucsik, Béla/0000-0002-1951-5974; Heincz, Adrián László/0000-0001-7563-0136}
}

@article{MTMT:3399845,
	title = {Pervasive early diagenetic dolomitization, subsequent hydrothermal alteration, and late stage hydrocarbon accumulation in a Middle Triassic carbonate sequence (Szeged Basin, SE Hungary)},
	url = {https://m2.mtmt.hu/api/publication/3399845},
	author = {Garaguly, István and Raucsikné Varga, Andrea Beáta and Raucsik, Béla and Schubert, Félix and Czuppon, György and Frei, R},
	doi = {10.1016/j.marpetgeo.2018.07.024},
	journal-iso = {MAR PETROL GEOL},
	journal = {MARINE AND PETROLEUM GEOLOGY},
	volume = {98},
	unique-id = {3399845},
	issn = {0264-8172},
	year = {2018},
	eissn = {1873-4073},
	pages = {270-290},
	orcid-numbers = {Garaguly, István/0000-0002-2802-0738; Raucsikné Varga, Andrea Beáta/0000-0002-8673-1482; Raucsik, Béla/0000-0002-1951-5974; Schubert, Félix/0000-0001-8647-5354; Czuppon, György/0000-0002-7231-6042}
}

@article{MTMT:3202162,
	title = {Középső-triász dolomitok képződésének története és töréses deformációja a Szegedi-medence területén},
	url = {https://m2.mtmt.hu/api/publication/3202162},
	author = {Garaguly, István and Raucsik, Béla and Raucsikné Varga, Andrea Beáta and Schubert, Félix},
	doi = {10.23928/foldt.kozl.2017.147.1.39},
	journal-iso = {FÖLDTANI KÖZLÖNY},
	journal = {FÖLDTANI KÖZLÖNY},
	volume = {147},
	unique-id = {3202162},
	issn = {0015-542X},
	year = {2017},
	eissn = {2559-902X},
	pages = {39-60},
	orcid-numbers = {Garaguly, István/0000-0002-2802-0738; Raucsik, Béla/0000-0002-1951-5974; Raucsikné Varga, Andrea Beáta/0000-0002-8673-1482; Schubert, Félix/0000-0001-8647-5354}
}

@article{MTMT:3304112,
	title = {A dorozsmai márvány (Tiszai-főegység) kőzettani újravizsgálata: deformáció és fluidum hatása a mikroszerkezet fejlődésére},
	url = {https://m2.mtmt.hu/api/publication/3304112},
	author = {Papp, Nikoletta and Raucsikné Varga, Andrea Beáta and Mészáros, Előd and Raucsik, Béla},
	doi = {10.23928/foldt.kozl.2017.147.4.337},
	journal-iso = {FÖLDTANI KÖZLÖNY},
	journal = {FÖLDTANI KÖZLÖNY},
	volume = {147},
	unique-id = {3304112},
	issn = {0015-542X},
	year = {2017},
	eissn = {2559-902X},
	pages = {337-356},
	orcid-numbers = {Raucsikné Varga, Andrea Beáta/0000-0002-8673-1482; Mészáros, Előd/0000-0002-5846-9034; Raucsik, Béla/0000-0002-1951-5974}
}

@article{MTMT:3132886,
	title = {Provenance of the Upper Triassic siliciclastics of the Mecsek Mountains and Villány Hills (Pannonian Basin, Hungary). constraints to the Early Mesozoic paleogeography of the Tisza Megaunit},
	url = {https://m2.mtmt.hu/api/publication/3132886},
	author = {Pozsgai, Emília and Józsa, Sándor and Dunkl, István and Sebe, Krisztina and Thamóné Bozsó, Edit and Sajó, István and Dezső, József and von Eynatten, H},
	doi = {10.1007/s00531-016-1406-0},
	journal-iso = {INT J EARTH SCI},
	journal = {INTERNATIONAL JOURNAL OF EARTH SCIENCES},
	volume = {106},
	unique-id = {3132886},
	issn = {1437-3254},
	abstract = {The Tisza Megaunit in the Southern Pannonian Basin formed part of the southern margin of the European Plate in the Early Mesozoic era. Its exact paleo-position and relation to other structural blocks is disputed for a long time. Detrital zircon U–Pb dating, heavy mineral analysis and petrographical examination of Carnian to Pliensbachian sandstone members lead to better understanding of the provenance of clastic deposits after the Ladinian–Carnian carbonate to siliciclastic facies shift in the Southwestern Tisza Megaunit. Investigations allow for constraining its paleogeographic relation to adjacent units. The Carnian and Pliensbachian siliciclastics of the Villány Hills derive from inside the Southwestern Tisza Megaunit, i.e. the medium-grade polymetamorphic rocks of the adjacent Slavonian Mountains or similar basement fragments. The Upper Triassic clastic deposits of the Mecsek Mountains most likely derive from Variscan felsic plutonic rocks of the local basement or partially from the Southern/Southwestern Bohemian Massif. About 200 Ma zircon U–Pb ages are tentatively interpreted as traces of synsedimentary distal volcanism in the Central Atlantic Magmatic Province.},
	keywords = {EVOLUTION; PROVENANCE; sandstones; BOHEMIAN MASSIF; U-PB; HEAVY MINERAL ANALYSIS; Tisza Megaunit; Upper Triassic; VARISCAN OROGEN; SOUTHERN HUNGARY; CHRONOLOGICAL CONSTRAINTS; HEAVY MINERAL ASSEMBLAGES; MEDITERRANEAN ALPINE CHAINS; Detrital zircon U-Pb geochronology; Zircon ages},
	year = {2017},
	eissn = {1437-3262},
	pages = {2005-2024},
	orcid-numbers = {Józsa, Sándor/0000-0001-8219-0044; Sebe, Krisztina/0000-0002-4647-2199; Sajó, István/0000-0002-1228-1407}
}

@article{MTMT:26390889,
	title = {Petrologic comparison of the Gyod and Helesfa serpentinite bodies (Tisia Mega Unit, SW Hungary)},
	url = {https://m2.mtmt.hu/api/publication/26390889},
	author = {Kovacs, Gabor and Radovics, Balázs Géza and M. Tóth, Tivadar},
	doi = {10.3190/jgeosci.218},
	journal-iso = {J GEOSCI},
	journal = {JOURNAL OF GEOSCIENCES},
	volume = {61},
	unique-id = {26390889},
	issn = {1802-6222},
	year = {2016},
	eissn = {1803-1943},
	pages = {255-279},
	orcid-numbers = {M. Tóth, Tivadar/0000-0003-1012-1095}
}

@article{MTMT:3156315,
	title = {A Gyűrűfűi Riolit Formáció kőzettani vizsgálata a felszíni előfordulások alapján (Nyugati-Mecsek)},
	url = {https://m2.mtmt.hu/api/publication/3156315},
	author = {Szemerédi, Máté and Raucsikné Varga, Andrea Beáta and Haranginé Lukács, Réka and Pál-Molnár, Elemér},
	journal-iso = {FÖLDTANI KÖZLÖNY},
	journal = {FÖLDTANI KÖZLÖNY},
	volume = {146},
	unique-id = {3156315},
	issn = {0015-542X},
	abstract = {The Permian Gyűrűfű Rhyolite Formation is the only volcanic 
		association within the Palaeozoic sequence of
		Southern Transdanubia which outcrops in the western foreland 
		of the Mecsek Mts. Furthermore, this formation has long
		been well-known as the source of the gravel material of the 
		younger sedimentary siliciclastic formations in the area. Due
		to the uranium ore exploration deep drillings of the second 
		half of the 20th century, details about the subsurface 
		regions of
		the formation are also well-documented; these regions include 
		the Western Mecsek Mts, the northern foreland of the
		Villány Mts and the Máriakéménd–Bár–Báta Range.
		According to the previous reports of uranium ore exploration 
		and other studies based on them (SZEDERKÉNYI 1962,
		BARABÁSNÉ STUHL 1988, FÜLÖP 1994, BARABÁS & BARABÁSNÉ STUHL 
		1998, JAKAB 2005), the material of the outcrop is
		a lava rock. In the early stage of the research only PANTÓ 
		(in BOCZÁN et al. 1966) mentioned the possibility of a 
		pyroclastic
		(ignimbrite) origin. The later petrographic descriptions of 
		the rocks recognised the common appearance of flattened,
		oriented pumices and this made it necessary to implement a 
		process of reambulation. As the first step in this process,
		HIDASI et al. (2015) documented detailed petrographic 
		descriptions of the deep-drilling and gravel material of the
		formation and, according his work, many textural features 
		indicate a pyroclastic flow origin.
		In this study, detailed macroscopic and microscopic 
		documentation is given of surficial samples of Gyűrűfű 
		Rhyolite
		(from area between the villages of Gyűrűfű and Dinnyeberki, 
		Western Mecsek Mts). Many textural features (e.g.
		devitrified pumices, former glass shards, poor sorting, 
		fragmented phenocrysts) of the pyroclastic flow deposits were
		also observed. In this paper the surficial rock material of 
		the formation is presented as an altered, locally strongly-
		welded,
		crystal-rich, pumice-bearing lapilli tuff. According to the 
		intensity of the welding, 2 lithofacies were distinguished. 
		The
		eutaxitic, strongly-welded rock samples could have their 
		origin in the medium or greater depth of the proximal part of 
		the
		pyroclastic flows; the latter filled a former valley in the 
		area of Gyűrűfű. The non-welded material is probably derived
		from the lowermost, upper, sideward or distal part of the 
		pyroclastic flows.
		Alongside the petrographic description, this study was 
		supplemented with preliminary zircon examinations as part
		of the preparations for U-Pb radiometric dating. From the 
		examined samples more than 200 pieces of zircon grains were
		documented. Based on this database, the respective zircon 
		populations of the two lithofacies were analysed and compared
		(using statistical parameters). Zircon crystals were found 
		both in the matrix and within the phenocrysts of the rock
		samples. The high amount of idiomorphic and hipidomorphic 
		zircon grains that appear in the groundmass shows the
		possibility of zircon crystallization within the rock-forming 
		magma. Most of the zircon grains are fragmented and this
		fact serves as further evidence of a pyroclastic origin. The 
		examined zircon crystals often show zonation and contain
		xenocrystic cores; these details need to be taken into 
		account when carrying out U-Pb radiometric dating.},
	year = {2016},
	eissn = {2559-902X},
	pages = {335-354},
	orcid-numbers = {Szemerédi, Máté/0000-0002-7432-8418; Raucsikné Varga, Andrea Beáta/0000-0002-8673-1482; Haranginé Lukács, Réka/0000-0002-2338-4209; Pál-Molnár, Elemér/0000-0002-9606-0133}
}

@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:2008179,
	title = {"Ízesítő" a permi Bodai Agyagkő Formáció őskörnyezeti rekonstrukciójához: kősó utáni pszeudomorfózák a BAT-4 fúrás agyagkőmintáiban},
	url = {https://m2.mtmt.hu/api/publication/2008179},
	author = {Máthé, Zoltán and Raucsikné Varga, Andrea Beáta},
	journal-iso = {FÖLDTANI KÖZLÖNY},
	journal = {FÖLDTANI KÖZLÖNY},
	volume = {142},
	unique-id = {2008179},
	issn = {0015-542X},
	year = {2012},
	eissn = {2559-902X},
	pages = {201-204},
	orcid-numbers = {Raucsikné Varga, Andrea Beáta/0000-0002-8673-1482}
}

@article{MTMT:1930795,
	title = {Cirkon egykristály U-Pb korok a danitzpusztai pannóniai homokból: közvetett bizonyítékok az aljzatot alkotó metamorfitok kevert prevariszkuszi protolitjaira},
	url = {https://m2.mtmt.hu/api/publication/1930795},
	author = {Raucsikné Varga, Andrea Beáta and Újvári, Gábor and Kovács, János},
	journal-iso = {FÖLDTANI KÖZLÖNY},
	journal = {FÖLDTANI KÖZLÖNY},
	volume = {142},
	unique-id = {1930795},
	issn = {0015-542X},
	year = {2012},
	eissn = {2559-902X},
	pages = {95-98},
	orcid-numbers = {Raucsikné Varga, Andrea Beáta/0000-0002-8673-1482; Újvári, Gábor/0000-0002-2816-6155; Kovács, János/0000-0001-7742-5515}
}

@article{MTMT:2008320,
	title = {On possible origin of background contents of heavy metals and metalloids in the subsurface Pennsylvanian Téseny metasandstones, SW Hungary},
	url = {https://m2.mtmt.hu/api/publication/2008320},
	author = {Raucsikné Varga, Andrea Beáta and Raucsik, Béla and Szakmány, György},
	journal-iso = {CARPATH J EARTH ENVIRON SCI},
	journal = {CARPATHIAN JOURNAL OF EARTH AND ENVIRONMENTAL SCIENCES},
	volume = {7},
	unique-id = {2008320},
	issn = {1842-4090},
	year = {2012},
	eissn = {1844-489X},
	pages = {211-218},
	orcid-numbers = {Raucsikné Varga, Andrea Beáta/0000-0002-8673-1482; Raucsik, Béla/0000-0002-1951-5974; Szakmány, György/0000-0002-9557-2030}
}

@article{MTMT:1687934,
	title = {The relevance of vein texture in understanding the past hydraulic behaviour of a crystalline rock mass: reconstruction of the palaeohydrology of the Mecsekalja Zone, south Hungary},
	url = {https://m2.mtmt.hu/api/publication/1687934},
	author = {Dabi, Gergely and Siklósy, Zoltán and Schubert, Félix and Bajnóczi, Bernadett and M. Tóth, Tivadar},
	doi = {10.1111/j.1468-8123.2011.00342.x},
	journal-iso = {GEOFLUIDS},
	journal = {GEOFLUIDS},
	volume = {11},
	unique-id = {1687934},
	issn = {1468-8115},
	year = {2011},
	eissn = {1468-8123},
	pages = {309-327},
	orcid-numbers = {Schubert, Félix/0000-0001-8647-5354; Bajnóczi, Bernadett/0000-0003-0006-7611; M. Tóth, Tivadar/0000-0003-1012-1095}
}

@article{MTMT:1722066,
	title = {Hydrothermal palaeofluid circulation in the fracture network of the Baksa Gneiss Complex of SW Pannonian Basin, Hungary.},
	url = {https://m2.mtmt.hu/api/publication/1722066},
	author = {Fintor, Krisztián and M. Tóth, Tivadar and Schubert, Félix},
	doi = {10.1111/j.1468-8123.2011.00327.x},
	journal-iso = {GEOFLUIDS},
	journal = {GEOFLUIDS},
	volume = {11},
	unique-id = {1722066},
	issn = {1468-8115},
	year = {2011},
	eissn = {1468-8123},
	pages = {144-165},
	orcid-numbers = {Fintor, Krisztián/0000-0003-4794-9419; M. Tóth, Tivadar/0000-0003-1012-1095; Schubert, Félix/0000-0001-8647-5354}
}

@article{MTMT:1343667,
	title = {Near vein metasomatism along propylitic veins in the Baksa Gneiss Complex, Pannonian Basin, Hungary},
	url = {https://m2.mtmt.hu/api/publication/1343667},
	author = {Fintor, Krisztián and M. Tóth, Tivadar and Schubert, Félix},
	doi = {10.4154/GC.2010.05},
	journal-iso = {GEOL CROAT},
	journal = {GEOLOGIA CROATICA},
	volume = {63},
	unique-id = {1343667},
	issn = {1330-030X},
	year = {2010},
	eissn = {1333-4875},
	pages = {75-91},
	orcid-numbers = {Fintor, Krisztián/0000-0003-4794-9419; M. Tóth, Tivadar/0000-0003-1012-1095; Schubert, Félix/0000-0001-8647-5354}
}

@article{MTMT:1348919,
	title = {Sedimentology of a Permian playa lake: the Boda Claystone Formation, Hungary},
	url = {https://m2.mtmt.hu/api/publication/1348919},
	author = {Konrád, Gyula and Sebe, Krisztina and Halász, Amadé and Babinszki, Edit},
	doi = {10.2478/v10118-010-0002-1},
	journal-iso = {GEOLOGOS},
	journal = {GEOLOGOS},
	volume = {16},
	unique-id = {1348919},
	issn = {1426-8981},
	abstract = {The Upper Permian Boda Claystone Formation (BCF) in SW Hungary has been previously been identified as a saline lake deposit. A country-wide screening found this 800–1000 m thick succession the most suitable for the disposal of high-level radioactive waste in Hungary, and research into this formation has consequently been intensified since. The investigations included a detailed study of the sedimentological characteristics. Data obtained by mapping of the 25 km2 outcrop area of the formation and from more than 40 boreholes were processed. The sedimentary structures were investigated on outcrop to microscopic scales, and cycles in the succession were interpreted.
		The main lithofacies, sedimentary structures and ichnofossils are presented. They indicate that the major part of the succession was deposited in a playa mudflat and is not of lacustrine origin in a strict sense. The lake sediments are represented
		by laminated and ripple-marked/flaser-type cross-laminated claystones and siltstones and by massive dolomites;
		trace fossils include crawling traces and burrows. Partial or complete drying out of the lake commonly occurred after the formation of carbonate mud by evaporation. Periodic fluvial influx is recorded by cross-bedded sandstones and unsorted gravelly sandstones of up to pebble-sized angular grains. Fenestral and stromatolitic structures reflect the repeated appearance of playa mudflat conditions. The silty claystones, which compose the major part of the succession, lost their primary structures due to pedogenic processes and indicate prolonged subaerial intervals with soil formation and only ephemeral inundations. The presence of pedogenic carbonate concretions supports the interpretation of an arid climate and a relatively shallow groundwater table. Drying-out events shown by desiccation cracks and authigenic breccias can be traced all over the succession.
		The various facies form small-scale sedimentary cycles showing a shallowing-upward trend and the growing influence of aridity and subaerial exposure.},
	year = {2010},
	eissn = {2080-6574},
	pages = {27-41},
	orcid-numbers = {Sebe, Krisztina/0000-0002-4647-2199; Halász, Amadé/0000-0003-4582-8883}
}

@inbook{MTMT:1382887,
	title = {A Baksai Komplexum posztmetamorf fluidum evolúciója},
	url = {https://m2.mtmt.hu/api/publication/1382887},
	author = {Fintor, Krisztián and M. Tóth, Tivadar and Schubert, Félix},
	booktitle = {Magmás és metamorf képződmények a Tiszai Egységben},
	unique-id = {1382887},
	year = {2009},
	pages = {245-258},
	orcid-numbers = {Fintor, Krisztián/0000-0003-4794-9419; M. Tóth, Tivadar/0000-0003-1012-1095; Schubert, Félix/0000-0001-8647-5354}
}

@article{MTMT:152130,
	title = {Late Variscan (Carboniferous to Permian) environments in the Circum Pannonian Region},
	url = {https://m2.mtmt.hu/api/publication/152130},
	author = {Vozarova, A and Ebner, F and Kovács, Sándor and Krautner, HG and Szederkenyi, T and Krstic, B and Sremac, J and Aljinovic, D and Novak, M and Skaberne, D},
	doi = {10.2478/v10096-009-0002-7},
	journal-iso = {GEOL CARPATH},
	journal = {GEOLOGICA CARPATHICA},
	volume = {60},
	unique-id = {152130},
	issn = {1335-0552},
	year = {2009},
	eissn = {1336-8052},
	pages = {71-104}
}

@article{MTMT:1129844,
	title = {Hiperszalin paleofluidum-áramlás nyomai a Baksai Komplexum repedésrendszerében},
	url = {https://m2.mtmt.hu/api/publication/1129844},
	author = {Fintor, Krisztián and Schubert, Félix and M. Tóth, Tivadar},
	journal-iso = {FÖLDTANI KÖZLÖNY},
	journal = {FÖLDTANI KÖZLÖNY},
	volume = {138},
	unique-id = {1129844},
	issn = {0015-542X},
	year = {2008},
	eissn = {2559-902X},
	pages = {257-278},
	orcid-numbers = {Fintor, Krisztián/0000-0003-4794-9419; Schubert, Félix/0000-0001-8647-5354; M. Tóth, Tivadar/0000-0003-1012-1095}
}

@{MTMT:1831361,
	title = {Complex examination of the Upper Paleozoic siliciclastic rocks from southern Transdanubia, SW Hungary - Mineralogical, petrographic, and geochemical study},
	url = {https://m2.mtmt.hu/api/publication/1831361},
	author = {Raucsikné Varga, Andrea Beáta and Szakmány, György and Árgyelán, T and Józsa, Sándor and Raucsik, Béla and Máthé, Zoltán},
	booktitle = {Sedimentary Provenance and Petrogenesis: Perspectives from Petrography and Geochemistry},
	doi = {10.1130/2006.2420(14)},
	unique-id = {1831361},
	year = {2007},
	pages = {221-240},
	orcid-numbers = {Raucsikné Varga, Andrea Beáta/0000-0002-8673-1482; Szakmány, György/0000-0002-9557-2030; Józsa, Sándor/0000-0001-8219-0044; Raucsik, Béla/0000-0002-1951-5974}
}

@article{MTMT:1302228,
	title = {Chemical composition, provenance and early diagenetic processes of playa lake deposits from the Boda Siltstone Formation (Upper Permian), SW Hungary},
	url = {https://m2.mtmt.hu/api/publication/1302228},
	author = {Raucsikné Varga, Andrea Beáta and Szakmány, György and Raucsik, Béla and Máthé, Zoltán},
	doi = {10.1556/AGeol.48.2005.1.2},
	journal-iso = {ACTA GEOL HUNG},
	journal = {ACTA GEOLOGICA HUNGARICA: A QUARTERLY OF THE HUNGARIAN ACADEMY OF SCIENCES},
	volume = {48},
	unique-id = {1302228},
	issn = {0236-5278},
	year = {2005},
	pages = {49-68},
	orcid-numbers = {Raucsikné Varga, Andrea Beáta/0000-0002-8673-1482; Szakmány, György/0000-0002-9557-2030; Raucsik, Béla/0000-0002-1951-5974}
}

@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: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:1019054,
	title = {Mesozoic evolution of the Tisza Mega-unit},
	url = {https://m2.mtmt.hu/api/publication/1019054},
	author = {Haas, János and Péró, Csaba},
	doi = {10.1007/s00531-004-0384-9},
	journal-iso = {INT J EARTH SCI},
	journal = {INTERNATIONAL JOURNAL OF EARTH SCIENCES},
	volume = {93},
	unique-id = {1019054},
	issn = {1437-3254},
	year = {2004},
	eissn = {1437-3262},
	pages = {297-313},
	orcid-numbers = {Haas, János/0000-0003-0929-8889}
}

@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:1203502,
	title = {A Siklósbodony Sb-1 mélyfúrás feltételezett karbon-perm határképződményeinek ásványtani, kőzettani és geokémiai jellemzői [Mineralogical, petrographie and geochemical characteristics of siliciclastic rocks from the supposed Carboniferous-Permian boundary in borehole Siklósbodony Sb-1, South-western Hungary]},
	url = {https://m2.mtmt.hu/api/publication/1203502},
	author = {Raucsikné Varga, Andrea Beáta and Raucsik, Béla and Szakmány, György},
	journal-iso = {FÖLDTANI KÖZLÖNY},
	journal = {FÖLDTANI KÖZLÖNY},
	volume = {134},
	unique-id = {1203502},
	issn = {0015-542X},
	year = {2004},
	eissn = {2559-902X},
	pages = {321-343},
	orcid-numbers = {Raucsikné Varga, Andrea Beáta/0000-0002-8673-1482; Raucsik, Béla/0000-0002-1951-5974; Szakmány, György/0000-0002-9557-2030}
}

@article{MTMT:1302237,
	title = {Geochemistry and provenance of the Upper Carboniferous sandstones from borehole Diósviszló-3 (Téseny Sandstone Formation, SW Hungary)},
	url = {https://m2.mtmt.hu/api/publication/1302237},
	author = {Raucsikné Varga, Andrea Beáta and Szakmány, György},
	journal-iso = {ACTA MINERAL PETROGR},
	journal = {ACTA MINERALOGICA PETROGRAPHICA},
	volume = {45},
	unique-id = {1302237},
	issn = {0365-8066},
	year = {2004},
	pages = {7-14},
	orcid-numbers = {Raucsikné Varga, Andrea Beáta/0000-0002-8673-1482; Szakmány, György/0000-0002-9557-2030}
}

@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:1303024,
	title = {A nyugat-mecseki alsó-miocén konglomerátum karbon homokkő kavicsainak és a Tésenyi Homokkő Formáció képződményeinek petrográfiai és geokémiai összehasonlítása},
	url = {https://m2.mtmt.hu/api/publication/1303024},
	author = {Raucsikné Varga, Andrea Beáta and Szakmány, György and Józsa, Sándor and Máthé, Zoltán},
	journal-iso = {FÖLDTANI KÖZLÖNY},
	journal = {FÖLDTANI KÖZLÖNY},
	volume = {131},
	unique-id = {1303024},
	issn = {0015-542X},
	year = {2001},
	eissn = {2559-902X},
	pages = {11-36},
	orcid-numbers = {Raucsikné Varga, Andrea Beáta/0000-0002-8673-1482; Szakmány, György/0000-0002-9557-2030; Józsa, Sándor/0000-0001-8219-0044}
}

@article{MTMT:1016511,
	title = {Composition, diagenetic and post-diagenetic alterations of a possible radioactive waste repository site: the Boda Albitic Claystone Formation, southern Hungary},
	url = {https://m2.mtmt.hu/api/publication/1016511},
	author = {Árkai, Péter and Demény, Attila and Fórizs, István and Nagy, Géza and Balogh, Kadosa and Máthé, Zoltán},
	journal-iso = {ACTA GEOL HUNG},
	journal = {ACTA GEOLOGICA HUNGARICA: A QUARTERLY OF THE HUNGARIAN ACADEMY OF SCIENCES},
	volume = {43},
	unique-id = {1016511},
	issn = {0236-5278},
	year = {2000},
	pages = {351-378},
	orcid-numbers = {Demény, Attila/0000-0003-0522-9018; Fórizs, István/0000-0003-0813-6079}
}

@article{MTMT:32178175,
	title = {Cimmerian and alpine stratigraphy and structural evolution of the moesian platform (Romania/Bulgaria)},
	url = {https://m2.mtmt.hu/api/publication/32178175},
	author = {Tari, Gábor and Dicea, O and Faulkerson, J and Georgiev, G and Popov, S and Stefanescu, M and Weir, G},
	journal-iso = {AAPG MEMOIR},
	journal = {AAPG MEMOIR},
	volume = {68},
	unique-id = {32178175},
	issn = {0271-8529},
	year = {1997},
	pages = {63-90}
}