@{MTMT:2145815,
	title = {Az Aggtelek-Rudabányai-hegység fedetlen földtani térképe M=1:25 000, 1988 (ISBN: 963 671 119 4 CI)},
	url = {https://m2.mtmt.hu/api/publication/2145815},
	author = {Less, György and Grill, J and Szentpétery, I and Róth, L and Gyuricza, György},
	booktitle = {Az Aggtelek–Rudabányai-hegység földtana},
	unique-id = {2145815},
	year = {2006},
	pages = {1 A/0-2 A/0}
}

@article{MTMT:152210,
	title = {Geological setting of Triassic "Hallstatt" (s.l.) facies in NE Hungary},
	url = {https://m2.mtmt.hu/api/publication/152210},
	author = {Péró, Csaba and Kovács, Sándor and Less, György and Fodor, László},
	journal-iso = {ANN UNIV SCI BP R EÖTVÖS NOM SECT GEOL},
	journal = {ANNALES UNIVERSITATIS SCIENTIARUM BUDAPESTINENSIS DE ROLANDO EÖTVÖS NOMINATAE - SECTIO GEOLOGICA},
	volume = {35},
	unique-id = {152210},
	issn = {0365-0634},
	year = {2003},
	pages = {58-60}
}

@article{MTMT:1155431,
	title = {Geodynamics of SW-Pannonian inselbergs (Mecsek and Villány Mts, SW Hungary): inferences from a complex structural analysis},
	url = {https://m2.mtmt.hu/api/publication/1155431},
	author = {Csontos, L and Márton Péterné Szalay, Emőke and Wórum, G and Benkovics, L},
	journal-iso = {EGU STEPHAN MUELLER SPEC PUBL SER},
	journal = {EGU STEPHAN MUELLER SPECIAL PUBLICATION SERIES},
	volume = {3},
	unique-id = {1155431},
	issn = {1868-4556},
	year = {2002},
	eissn = {1868-4564},
	pages = {1-19},
	orcid-numbers = {Márton Péterné Szalay, Emőke/0000-0002-2135-8867}
}

@article{MTMT:1621179,
	title = {Connection of neogene basin formation, magmatism and cooling of metamorphics in NE Slovenia.},
	url = {https://m2.mtmt.hu/api/publication/1621179},
	author = {Fodor, László and Jelen, B and Márton Péterné Szalay, Emőke and Zupancic, N and Trajanova, M and Rifelj, H and Pécskay, Zoltán and Balogh, Kadosa and Koroknai, B and Dunkl, István and Horváth, Péter and Horvat, A and Vrabec, M and Kraljic, M and Kevric, R},
	journal-iso = {GEOL CARPATH},
	journal = {GEOLOGICA CARPATHICA},
	volume = {53},
	unique-id = {1621179},
	issn = {1335-0552},
	keywords = {Earth, Cosmic and Environm. Res.,},
	year = {2002},
	eissn = {1336-8052},
	pages = {199-201},
	orcid-numbers = {Márton Péterné Szalay, Emőke/0000-0002-2135-8867}
}

@article{MTMT:1042243,
	title = {In the wake of a countercklockwise rotating Adriatic microplate: Neogene paleomagnetic results from northern Croatia},
	url = {https://m2.mtmt.hu/api/publication/1042243},
	author = {Márton Péterné Szalay, Emőke and Pavelić, D and Tomljenović, B and Avanić, R and Pamić, J and Márton, Péter},
	doi = {10.1007/s00531-001-0249-4},
	journal-iso = {INT J EARTH SCI},
	journal = {INTERNATIONAL JOURNAL OF EARTH SCIENCES},
	volume = {91},
	unique-id = {1042243},
	issn = {1437-3254},
	year = {2002},
	eissn = {1437-3262},
	pages = {514-523},
	orcid-numbers = {Márton Péterné Szalay, Emőke/0000-0002-2135-8867}
}

@article{MTMT:2899897,
	title = {Neogene-quaternary structures in the border zone between Alps, Dinarides and Pannonian Basin (Hrvatsko zagorje and Karlovac Basins, Croatia)},
	url = {https://m2.mtmt.hu/api/publication/2899897},
	author = {Tomljenovic, B and Csontos, László},
	doi = {10.1007/s005310000176},
	journal-iso = {INT J EARTH SCI},
	journal = {INTERNATIONAL JOURNAL OF EARTH SCIENCES},
	volume = {90},
	unique-id = {2899897},
	issn = {1437-3254},
	abstract = {Analysis of Neogene-Quaternary structures from seismic lines, surface measurements and geological-mapping is presented from the border zone between the Alps, Dinarides and Pannonian Basin. First, Early Miocene extension was possibly characterised by ENE directed extension. It was partly synchronous with NW-SE shortening. Second, Middle Miocene extension was possibly characterised by NW-SE to WNW-ESE directed extension. Again, this event was followed by a new generation of thrusts related to end-Sarmatian shortening. The last, Late Miocene E-W to WNW-ESE directed extension was followed by a final shortening that created major, map-scale folds, basement pop-ups and inverted former basins. Geometry, onlap and thickness patterns of the youngest syn-tectonic basin fill indicate that this last, N-S to NW-SE directed shortening started in Late Pontian and continued up to the present time. When taking into account the wider surrounding area, it seems that the structures related to this latest shortening are arranged in often perpendicular directions, centred at the eastern end of the Periadriatic lineament. To explain this fan-like pattern of synchronous shortenings a kinematic model is proposed combining counter-clockwise rotation with north- or northwestward shift of the Dinaridic block with respect to the more stable Alpine buttress.},
	year = {2001},
	eissn = {1437-3262},
	pages = {560-578}
}

@article{MTMT:21052,
	title = {Paleobiogeographical analysis: a tool for the reconstruction of Mesozoic Tethyan and Penninic basins},
	url = {https://m2.mtmt.hu/api/publication/21052},
	author = {Vörös, Attila},
	journal-iso = {ACTA GEOL HUNG},
	journal = {ACTA GEOLOGICA HUNGARICA: A QUARTERLY OF THE HUNGARIAN ACADEMY OF SCIENCES},
	volume = {44},
	unique-id = {21052},
	issn = {0236-5278},
	year = {2001},
	pages = {145-158}
}

@article{MTMT:1019043,
	title = {Complex structural pattern of the Alpine-Dinaridic-Pannonian triple junction},
	url = {https://m2.mtmt.hu/api/publication/1019043},
	author = {Haas, János and P, Mioć and J, Pamić and B, Tomljenović and Árkai, Péter and A, Bérczi-Makk and Kovács, Sándor and B, Koroknai and E, Rálisch-Felgenhauer},
	doi = {10.1007/s005310000093},
	journal-iso = {INT J EARTH SCI},
	journal = {INTERNATIONAL JOURNAL OF EARTH SCIENCES},
	volume = {89},
	unique-id = {1019043},
	issn = {1437-3254},
	year = {2000},
	eissn = {1437-3262},
	pages = {377-389},
	orcid-numbers = {Haas, János/0000-0003-0929-8889}
}

@article{MTMT:152233,
	title = {Tectonostratigraphic terranes in the pre-Neogene basement of the Hungarian part of the Pannonian area},
	url = {https://m2.mtmt.hu/api/publication/152233},
	author = {Kovács, Sándor and Szederkényi, T and Haas, János and Buda, György and Császár, Géza and Nagymarosy, András},
	journal-iso = {ACTA GEOL HUNG},
	journal = {ACTA GEOLOGICA HUNGARICA: A QUARTERLY OF THE HUNGARIAN ACADEMY OF SCIENCES},
	volume = {43},
	unique-id = {152233},
	issn = {0236-5278},
	year = {2000},
	pages = {225-328},
	orcid-numbers = {Haas, János/0000-0003-0929-8889}
}

@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}
}

@CONFERENCE{MTMT:152208,
	title = {Correlation of the Carboniferous, Permian and Triassic sequences of the Jadar Block, Sana-Una and "Bükkium" Terranes},
	url = {https://m2.mtmt.hu/api/publication/152208},
	author = {Protic, L and Filipovic, I and Pelikán, P and Jovanovic, D and Kovács, Sándor and Sudar, M and Hips, Kinga and Less, György and Cvijic, R},
	booktitle = {Proceedings of the International Symposium Geology and Metallogeny of the Dinarides and the Vardar Zone},
	unique-id = {152208},
	year = {2000},
	pages = {61-69},
	orcid-numbers = {Hips, Kinga/0000-0003-2315-120X}
}

@inbook{MTMT:1369059,
	title = {Tertiary tectonic evolution of the Pannonian Basin system and neighbouring orogens: a new synthesis of palaeostress data},
	url = {https://m2.mtmt.hu/api/publication/1369059},
	author = {Fodor, László and Csontos, L and Bada, G and Györfi, I and Benkovics, L},
	booktitle = {The Mediterranean Basins: tertiary extension within the Alpine Orogen},
	doi = {10.1144/GSL.SP.1999.156.01.15},
	unique-id = {1369059},
	year = {1999},
	pages = {295-334}
}

@article{MTMT:1042282,
	title = {First palaeo-magnetic results on Tertiary rocks from the Slavonian Mountains in the southern Pannonian basin, Crotia},
	url = {https://m2.mtmt.hu/api/publication/1042282},
	author = {Márton Péterné Szalay, Emőke and Pavelić, D and Tomljenović, B and Pamić, J and Márton, Péter},
	journal-iso = {GEOL CARPATH},
	journal = {GEOLOGICA CARPATHICA},
	volume = {50},
	unique-id = {1042282},
	issn = {1335-0552},
	year = {1999},
	eissn = {1336-8052},
	pages = {273-279},
	orcid-numbers = {Márton Péterné Szalay, Emőke/0000-0002-2135-8867}
}

@article{MTMT:1042273,
	title = {Tectonic aspects of a palaeomagnetic study on the Neogene of the Mecsek Mountains},
	url = {https://m2.mtmt.hu/api/publication/1042273},
	author = {Márton Péterné Szalay, Emőke and Márton, Péter},
	journal-iso = {GEOFIZIKAI KÖZLEMÉNYEK},
	journal = {GEOFIZIKAI KÖZLEMÉNYEK - GEOPHYSICAL TRANSACTIONS},
	volume = {42},
	unique-id = {1042273},
	issn = {0016-7177},
	year = {1999},
	pages = {159-180},
	orcid-numbers = {Márton Péterné Szalay, Emőke/0000-0002-2135-8867}
}

@article{MTMT:1256307,
	title = {Lithospheric structure of the Pannonian basin derived from seismic, gravity and geothermal data},
	url = {https://m2.mtmt.hu/api/publication/1256307},
	author = {Tari, Gábor and Dövényi, Péter and Dunkl, István and Horváth, Ferenc and Lenkey, László and Szafian, P and Toth, T},
	doi = {10.1144/GSL.SP.1999.156.01.12},
	journal-iso = {GEOL SOC SPEC PUBL},
	journal = {GEOLOGICAL SOCIETY SPECIAL PUBLICATIONS},
	volume = {156},
	unique-id = {1256307},
	issn = {0305-8719},
	abstract = {This paper is part of the special publication No.156, The Mediterranean basins: Tertiary extension within the Alpine Orogen. (eds B.Durand, L. Jolivet, F.Horvath and M.Seranne). The structure of the Pannonian basin is the result of distinct modes of Mid-Late Miocene extension exerting a profound effect on the lithospheric configuration, which continues even today. As the first manifestation of extensional collapse, large magnitude, metamorphic core complex style extension took place at the beginning of the Mid-Miocene in certain parts of the basin. Extrapolation of the present-day high heat flow in the basin, corrected for the blanketing effect of the basin fill, indicates a hot and thin lithosphere at the onset of extension. This initial condition, combined with the relatively thick crust inherited from earlier Alpine compressional episodes, appears to be responsible for the core complex type extension at the beginning of the syn-rift period. This type of extension is well documented in the northwestern Pannonian basin. Newly obtained deep reflection seismic and fission-track data integrated with well data from the southeastern part of the basin suggests that it developed in a similar fashion. Shortly after the initial period, the style of syn-rift extension changed to a wide-rift style, covering an area of much larger geographic extent. The associated normal faults revealed by industry reflection seismic data tend to dominate within the upper crust, obscuring pre-existing structures. However, several deep seismic profiles, constrained by gravity and geothermal modeling, image the entire lithosphere beneath the basin. It is the Mid-Miocene synrift extension which is still reflected in the structure of the Pannonian lithosphere, on the scale of the whole basin system. The gradually diminishing extension during the Late Miocene/Pliocene could not advance to the localization of extension into narrow rift zones in the Pannonian region except some deep subbasins such as the Mako/Bekes and Danube basins. These basins are underlain coincidently by anomalously thin crust (22-25 km) and lithosphere (45-60 km). Significant departures (up to 130 mW m -2) from the average present-day surface heat flow for the initiation of two newly defined narrow rift zones (Tisza and Duna) in the Pannonian basin system. However, both of these narrow rifts failed since the final docking of the Eastern Carpathians onto the European foreland excluded any further extension of the back-arc region.},
	year = {1999},
	eissn = {2041-4927},
	pages = {215-250},
	orcid-numbers = {Lenkey, László/0000-0003-4236-4075}
}

@article{MTMT:20066690,
	title = {Törmelékes krómspinellek a gerecsei jura képződményekben.},
	url = {https://m2.mtmt.hu/api/publication/20066690},
	author = {B, Árgyelán G and Császár, Géza},
	journal-iso = {FÖLDTANI KÖZLÖNY},
	journal = {FÖLDTANI KÖZLÖNY},
	volume = {128},
	unique-id = {20066690},
	issn = {0015-542X},
	year = {1998},
	eissn = {2559-902X},
	pages = {321-360}
}

@article{MTMT:1155176,
	title = {Miocene-Pliocene tectonic evolution of the Slovenian Periadriatic Line and surrounding area - Implications for Alpine-Carpathian extrusion models},
	url = {https://m2.mtmt.hu/api/publication/1155176},
	author = {Fodor, László and Jelen, B and Márton Péterné Szalay, Emőke and Skaberne, D and Čar, J and Vrabec, M},
	doi = {10.1029/98TC01605},
	journal-iso = {TECTONICS},
	journal = {TECTONICS},
	volume = {17},
	unique-id = {1155176},
	issn = {0278-7407},
	year = {1998},
	eissn = {1944-9194},
	pages = {690-709},
	orcid-numbers = {Márton Péterné Szalay, Emőke/0000-0002-2135-8867}
}

@article{MTMT:132435,
	title = {Palinspastic reconstruction and topographic evolution of the Eastern Alps during late Tertiary extrusion},
	url = {https://m2.mtmt.hu/api/publication/132435},
	author = {Frisch, W and Kuhlemann, J and Dunkl, István and Brügel, A},
	doi = {10.1016/S0040-1951(98)00160-7},
	journal-iso = {TECTONOPHYSICS},
	journal = {TECTONOPHYSICS},
	volume = {297},
	unique-id = {132435},
	issn = {0040-1951},
	year = {1998},
	eissn = {1879-3266},
	pages = {1-15}
}

@inbook{MTMT:1155180,
	title = {Palinspastic reconstruction of the Carpathian - Pannonian region during the Miocene.},
	url = {https://m2.mtmt.hu/api/publication/1155180},
	author = {Kováč, M and Nagymarosy, András and Oszczypko, N and Csontos, L and Slaczka, A and Marunteanu, M and Matenco, L and Márton Péterné Szalay, Emőke},
	booktitle = {Geodynamic development of the Western Carpathians},
	unique-id = {1155180},
	year = {1998},
	pages = {189-217},
	orcid-numbers = {Márton Péterné Szalay, Emőke/0000-0002-2135-8867}
}

@article{MTMT:1155168,
	title = {The bending model of the Transdanubian Central Range (Hungary) in the light of Triassic palaeomagnetic data},
	url = {https://m2.mtmt.hu/api/publication/1155168},
	author = {Márton Péterné Szalay, Emőke},
	doi = {10.1046/j.1365-246x.1998.00598.x},
	journal-iso = {GEOPHYS J INT},
	journal = {GEOPHYSICAL JOURNAL INTERNATIONAL},
	volume = {134},
	unique-id = {1155168},
	issn = {0956-540X},
	year = {1998},
	eissn = {1365-246X},
	pages = {625-633},
	orcid-numbers = {Márton Péterné Szalay, Emőke/0000-0002-2135-8867}
}

@article{MTMT:1021656,
	title = {Jurassic palaeogeography of the Transdanubian Central Range (Hungary)},
	url = {https://m2.mtmt.hu/api/publication/1021656},
	author = {Vörös, Attila and Galácz, András},
	doi = {10.13130/2039-4942/6112},
	journal-iso = {RIV IT PALEON STRATIG},
	journal = {RIVISTA ITALIANA DI PALEONTOLOGIA E STRATIGRAFIA},
	volume = {104},
	unique-id = {1021656},
	issn = {0035-6883},
	abstract = {The Transdanubian Central Range (TCR) is a flattened range of hills in northern Transdanubia (Hungary), formed mainly by Mesozoic carbonate rocks showing strong facies similarities with the Southern Alps and the Austroalpine domain. The Jurassic system is divided into several formations of predominantly pelagic limestones. Ammonoids are frequent and were collected bed-by-bed in numerous sections, providing an excellent biostratigraphic resolution. The thickness of the Jurassic system is usually small but changes along the strike of the TCR. It reaches a maximum thickness of 500 m in the western part; is very variable (10-400 m) in the central segment (Bakony Mts.) and rather low (less than 100 m) in the east (Gerecse). In the Bakony segment, the thickness variation reflects the strongly dissected topography of the Jurassic sea-floor. Synsedimentary tectonics is dominated by normal faults; tilted blocks and listric faults may be inferred only in the east.
		
		Five main steps were identified in the palaeogeographic evolution:
		
		1) Late Hettangian: carbonate oolitic shoals prevail, except for a few sites where non-deposition or neritic sediments occur.
		
		2) Sinemurian and Pliensbachian: tectonic disintegration resulted in an intricate pattern of submarine horsts and intervening basins, with condensed sedimentation or non-deposition on the horsts and thicker, continuous sedimentary sequences in the basins. The submarine topographic highs are surrounded by aprons of redeposited material (scarp breccias, brachiopod coquinas, crinoida calcarenites, spiculitic cherry limestones), while pure or argillaceous limestones (Rosso Ammonitico) prevail in the distal areas.
		
		3) Early Toarcian: the Tethys-wide anoxic event is superimposed on the previous submarine bottom topography; the resulting black shales and sedimentary Mn-ores are concentrated on the western sides of some horsts.
		
		4) Dogger to Early Maim: radiolarites with heterochronous lower and upper boundaries (Aalenian to Kimmeridgian) prevail, except for the top of some submarine topographic highs. The absence of uppermost Bathonian to Lower Oxfordian carbonates suggests that the whole TCR sunk below the CCD in those times.
		
		5) Latest Jurassic: the uniform deposition of Rosso Ammonitico and Biancone in the Late Kimmeridgian and Tithonian is interrupted only in the Early Tithonian by local intercalations of scarp breccias and coarse biodetrital limestones. This is interpreted as the last manifestation of synsedimentary tectonic movements along the faults bordering the submarine horsts.
		
		Based on palaeogeographic similarities and analogies in Jurassic times, the TCR is visualized as the northern foreground of the Trento platform/plateau (lying north of the later Insubric lineament), where the block-tectonic disintegration and differential subsidence started earlier and resulted in a bottom morphology more dissected than in the South Alpine part of this west Tethyan passive margin.},
	year = {1998},
	eissn = {2039-4942},
	pages = {69-84}
}

@article{MTMT:1016488,
	title = {Exhumation of the Rechnitz Window at the border of the Eastern Alps and Pannonian basin during Neogene extension. ALCAPA II Conference on Tectonics of the Alpine-Carpathian-Pannonian Region, COVASNA, ROMANIA, OCT 14-24, 1994},
	url = {https://m2.mtmt.hu/api/publication/1016488},
	author = {Dunkl, István and Demény, Attila},
	doi = {10.1016/S0040-1951(96)00258-2},
	journal-iso = {TECTONOPHYSICS},
	journal = {TECTONOPHYSICS},
	volume = {272},
	unique-id = {1016488},
	issn = {0040-1951},
	year = {1997},
	eissn = {1879-3266},
	pages = {197-211},
	orcid-numbers = {Demény, Attila/0000-0003-0522-9018}
}

@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}
}

@article{MTMT:1138169,
	title = {Tertiary brittle faulting and stress field evolution in the Gerecse Mountains, northern Hungary},
	url = {https://m2.mtmt.hu/api/publication/1138169},
	author = {Bada, G and Fodor, László and Székely, Balázs and Timár, Gábor},
	doi = {10.1016/0040-1951(95)00141-7},
	journal-iso = {TECTONOPHYSICS},
	journal = {TECTONOPHYSICS},
	volume = {255},
	unique-id = {1138169},
	issn = {0040-1951},
	abstract = {The Gerecse Mountains of the Transdanubian Range in northern 
		Hungary have suffered polyphase deformation during the Tertiary. 
		The evolution of the stress fields was determined by the 
		detailed structural survey of the area: the statistical analysis 
		of microtectonic observations, the mapping and reinterpretation 
		of fault pattern and the study of basin stratigraphy and 
		geometry. The stress fields show an apparent clockwise rotation 
		from Eocene until Quaternary times. Three main phases were 
		reconstructed. During the Eocene-Early Oligocene E-W- to ENE-
		WSW-oriented compression and perpendicular tension affected the 
		area. The formation and evolution of several sedimentary basins 
		were controlled by fault systems activated by this phase. After 
		a period of intensive erosion in the Early Oligocene the stress 
		field rotated approx, 30–40°: NW-SE-directed compression and NE-
		SW-trending tension existed during the Late Oligocene and Early 
		Miocene. After correction with palaeomagnetic data, an original 
		Palaeogene σ1 orientation is deduced NNE-SSW, reflecting the 
		collisional processes of Europe and the Apulian microplate. The 
		Middle Miocene to Pliocene period was characterised mainly by 
		extensional deformation: the direction of the minimal stress 
		axis (σ3) varied between E-W and NW-SE. The characteristic 
		clockwise rotation pattern of the Tertiary palaeostress fields 
		in the Gerecse Mts. is explained by the combined effect of the 
		regional stress field changes in the Carpatho-Pannonian region 
		and the rotation of the North Pannonian Unit.},
	keywords = {DEFORMATION; Tertiary; stress field; Hungary, Gerecse Mountains; tectonic rotation; brittle faulting},
	year = {1996},
	eissn = {1879-3266},
	pages = {269-289},
	orcid-numbers = {Székely, Balázs/0000-0002-6552-4329; Timár, Gábor/0000-0001-9675-6192}
}

@article{MTMT:1412630,
	title = {Mesozoic igneous suites in Hungary: Implications for genesis and tectonic setting in the northwestern part of Tethys},
	url = {https://m2.mtmt.hu/api/publication/1412630},
	author = {Harangi, Szabolcs and Szabó, Csaba and Józsa, Sándor and Szoldán, Z and Árva-Sós, Erzsébet and Balla, Márta and Kubovics, Imre},
	doi = {10.1080/00206819709465339},
	journal-iso = {INT GEOL REV},
	journal = {INTERNATIONAL GEOLOGY REVIEW},
	volume = {38},
	unique-id = {1412630},
	issn = {0020-6814},
	abstract = {Mesozoic igneous rocks occur in various tectonic units of the Intra-Carpathian Area of Eastern Europe. These rocks were situated several hundred km apart from one another during their formation, and subsequent large lateral displacements resulted in their present positions. They formed during a relatively wide temporal range (Middle Triassic to Late Cretaceous) through different petrogenetic processes associated with the Mesozoic evolution of the northwestern part of Tethys. In the Transdanubian subunit of the Alcapa block, Middle Triassic calc-alkaline, intermediateto-acidic, and potassic rocks occur as pyroclastics, lava flows, and dikes in the Bakony and Buda mountains. The Gemer-Bükk subunit of the Alcapa block comprises two different igneous series: (1) slightly metamorphosed Middle Triassic volcanic rocks of the Eastern Bükk Mountains, which can be divided into an older (Anisian-Early Ladinian) calc-alkaline, intermediateto-acidic volcanic series and a younger (Late Ladinian) alkaline basaltic series; and (2) two series of the Middle Triassic to Middle Jurassic ophiolite complex (Bódva Magmatic Series and Darnó-Szarvaskö Magmatic Series), embedded in a tectonic mélange and in an olistostrome suite along a SW-NE-oriented zone. The Tisza block contains Early Cretaceous alkaline volcanic rocks in the Mecsek-Alföld subunit. Strong temporal and geochemical correlations have been observed between the Middle Triassic volcanic rocks of the Bakony and Buda mountains and the Southern Alps, and those of the Eastern Bükk Mountains and the Outer Dinarides. We propose that all these rocks were formed during the same extension-related volcanic activity along the Southern Alps-Bakony and Buda mountains-Eastern Bükk Mountains-Dinarides region. The Middle Triassic-Middle Jurassic ultramafic-mafic igneous rocks of the Gemer-Bükk subunit can be correlated with the ophiolites of the Inner Dinarides. Geochemistry of the mafic rocks is consistent with an origin from an N-MORB and E-MORB source mantle. The Middle to Late Triassic ultramafic and mafic rocks of the Bódva and Darnó-Szarvaskö series could have originated along the mid-oceanic ridge system of the northwestern segment of the Vardar ocean (Meliaticum). The Middle Jurassic igneous rocks of the Darnó-Szarvaskö series could have corresponded to the opening of a backarc basin. Early Cretaceous alkaline volcanic rocks of the Mecsek-Alföld zone in the Tisza block formed as a result of continental rifting along the southern margin of the European plate. Two volcanic series - a mafic and a sodic group - were generated from an OIB-like asthenospheric mantle. Separation of the Tisza block from the European plate occurred contemporaneously with volcanic activity during the late Early Cretaceous.},
	keywords = {Hungary; tectonic setting; Tethys; igneous rock; Mesozoic; petrogenesis},
	year = {1996},
	eissn = {1938-2839},
	pages = {336-360},
	orcid-numbers = {Harangi, Szabolcs/0000-0003-2372-4581; Szabó, Csaba/0000-0002-1580-6344; Józsa, Sándor/0000-0001-8219-0044}
}

@article{MTMT:1098670,
	title = {Main Features of The Regional Metamorphic Events in Hungary: A Review},
	url = {https://m2.mtmt.hu/api/publication/1098670},
	author = {Lelkes-Felvari, G and Árkai, Péter and Sassi, FP and Balogh, Kadosa},
	journal-iso = {GEOL CARPATH},
	journal = {GEOLOGICA CARPATHICA},
	volume = {47},
	unique-id = {1098670},
	issn = {1335-0552},
	abstract = {The present paper reviews data concerning the crystalline basement of all tectonic units in Hungary. Their lithologic content, biostratigraphic data, metamorphic features and radiometric age data are presented and critically discussed. The effects of at least two regional metamorphic cycles have been definitely recognized, Alpine and Variscan, and some polymetamorphic situations suggest the possible existence of a third, older event. The following main events are distinguished: the Alpine, the Variscan and an early Variscan or pre-Variscan stage or event. Alpine metamorphism turns out to be more widespread than previously reported. The Alpine metamorphic grade ranges from subgreenschist to greenschist facies conditions, locally reaching the lower amphibolite facies. Low to medium pressure conditions have been generally ascertained for it, with local exceptions of high and transitional medium to high pressure conditions. The Variscan metamorphism has been detected in the majority of the pre-Permian rock sequences in Hungary. Its metamorphic grade covers the whole temperature field of metamorphism, up to anatectic conditions. The pressure conditions in the monometamorphi. Variscan low grade metapelites turn out to be low, related to a thermal gradient close to 40 degrees C/km. A pre-Alpine polymetamorphic character is displayed by some Variscan amphibolite facies metapelites. The youngest mineral assemblages in them are characterized by the occurrence of andalusite in the rocks of suitable bulk composition, displaying a low-pressure character of the Variscan event, consistently with the above reported pressure estimate inferred from the greenschist facies monometamorphic metapelites. The oldest mineral assemblage is characterized by the occurrence of kyanite in rocks of suitable bulk composition, which may be either referred to an early Variscan stage or to a pre-Variscan event.},
	year = {1996},
	eissn = {1336-8052},
	pages = {257-270}
}

@inbook{MTMT:1057109,
	title = {Large scale rotations in North Hungary during the Neogene as indicated by palaeomagnetic data},
	url = {https://m2.mtmt.hu/api/publication/1057109},
	author = {Márton Péterné Szalay, Emőke and Márton, Péter},
	booktitle = {Palaeomagnetism and Tectonics of the Mediterranean Region},
	unique-id = {1057109},
	year = {1996},
	pages = {153-173},
	orcid-numbers = {Márton Péterné Szalay, Emőke/0000-0002-2135-8867}
}

@article{MTMT:1098522,
	title = {Timing of low-temperature metamorphism and cooling of the Paleozoic and Mesozoic formations of the Bükkium, innermost Western Carpathians, Hungary},
	url = {https://m2.mtmt.hu/api/publication/1098522},
	author = {Árkai, Péter and Balogh, Kadosa and Dunkl, István},
	doi = {10.1007/BF00260444},
	journal-iso = {GEOL RUNDSCH},
	journal = {GEOLOGISCHE RUNDSCHAU},
	volume = {84},
	unique-id = {1098522},
	issn = {0016-7835},
	year = {1995},
	pages = {334-344}
}

@article{MTMT:1368438,
	title = {FROM TRANSPRESSION TO TRANSTENSION - OLIGOCENE MIOCENE STRUCTURAL EVOLUTION OF THE VIENNA BASIN AND THE EAST ALPINE WESTERN CARPATHIAN JUNCTION},
	url = {https://m2.mtmt.hu/api/publication/1368438},
	author = {Fodor, László},
	doi = {10.1016/0040-1951(94)00158-6},
	journal-iso = {TECTONOPHYSICS},
	journal = {TECTONOPHYSICS},
	volume = {242},
	unique-id = {1368438},
	issn = {0040-1951},
	year = {1995},
	eissn = {1879-3266},
	pages = {151-182}
}

@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:1155117,
	title = {Combination of palaeomagnetic and stress data - a case study from North Hungary.},
	url = {https://m2.mtmt.hu/api/publication/1155117},
	author = {Márton Péterné Szalay, Emőke and Fodor, László},
	doi = {10.1016/0040-1951(94)00153-Z},
	journal-iso = {TECTONOPHYSICS},
	journal = {TECTONOPHYSICS},
	volume = {242},
	unique-id = {1155117},
	issn = {0040-1951},
	year = {1995},
	eissn = {1879-3266},
	pages = {99-114},
	orcid-numbers = {Márton Péterné Szalay, Emőke/0000-0002-2135-8867}
}

@article{MTMT:1155128,
	title = {Escape models of the Alpine-Carpathian-Pannonian region in the light of palaeomagnetic observations.},
	url = {https://m2.mtmt.hu/api/publication/1155128},
	author = {Mauritsch, H and Márton Péterné Szalay, Emőke},
	doi = {10.1111/j.1365-3121.1995.tb00666.x},
	journal-iso = {TERRA NOVA},
	journal = {TERRA NOVA},
	volume = {7},
	unique-id = {1155128},
	issn = {0954-4879},
	year = {1995},
	eissn = {1365-3121},
	pages = {44-50},
	orcid-numbers = {Márton Péterné Szalay, Emőke/0000-0002-2135-8867}
}

@article{MTMT:132359,
	title = {Late Cretaceous exhumation of the metamorphic Gleinalm Dome, Eastern Alps: kinematics, cooling history, and sedimentary response in a sinistral wrench corridor},
	url = {https://m2.mtmt.hu/api/publication/132359},
	author = {Neubauer, F and Dallmeyer, RD and Dunkl, István and Schirnik, D},
	doi = {10.1016/0040-1951(94)00154-2},
	journal-iso = {TECTONOPHYSICS},
	journal = {TECTONOPHYSICS},
	volume = {242},
	unique-id = {132359},
	issn = {0040-1951},
	year = {1995},
	eissn = {1879-3266},
	pages = {79-98}
}

@article{MTMT:1447557,
	title = {Stratigraphic and micromineralogic investigations on Cretaceous formations of the Gerecse Mountains, Hungary and their palaeogeographic implications},
	url = {https://m2.mtmt.hu/api/publication/1447557},
	author = {Császár, Géza and Árgyelán, GB},
	doi = {10.1006/cres.1994.1024},
	journal-iso = {CRETACEOUS RES},
	journal = {CRETACEOUS RESEARCH},
	volume = {15},
	unique-id = {1447557},
	issn = {0195-6671},
	year = {1994},
	eissn = {1095-998X},
	pages = {417-434}
}

@article{MTMT:1155109,
	title = {Alpine uplift history of the Central Western Carpathians: geochronological, paleomagnetic, sedimantary and structural data.},
	url = {https://m2.mtmt.hu/api/publication/1155109},
	author = {Kováč, M and Král', J and Márton Péterné Szalay, Emőke and Plašienka, D and Uher, P},
	journal-iso = {GEOL CARPATH},
	journal = {GEOLOGICA CARPATHICA},
	volume = {45},
	unique-id = {1155109},
	issn = {1335-0552},
	year = {1994},
	eissn = {1336-8052},
	pages = {83-96},
	orcid-numbers = {Márton Péterné Szalay, Emőke/0000-0002-2135-8867}
}

@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:1255446,
	title = {TOWARDS A MECHANICAL MODEL FOR THE FORMATION OF THE PANNONIAN BASIN},
	url = {https://m2.mtmt.hu/api/publication/1255446},
	author = {Horváth, Ferenc},
	doi = {10.1016/0040-1951(93)90126-5},
	journal-iso = {TECTONOPHYSICS},
	journal = {TECTONOPHYSICS},
	volume = {226},
	unique-id = {1255446},
	issn = {0040-1951},
	abstract = {New maps showing crustal and lithospheric thickness variations in the
		Pannonian basin and the surrounding East Alpine, Carpathian and Dinaric
		mountains have been prepared on the basis of recent seismic,
		seismologic and electromagnetic data. A map presenting Miocene faults
		of regional significance has been also constructed for the same region
		by using a wealth of recently available national and/or more local
		studies. It is suggested that observed crustal and lithospheric
		structural contrasts have been controlled primarily by Neogene
		kinematic history of the region. Kinematic history is characterized by
		the following main patterns: (1) indentation by Adria and large-scale
		backthrusting in the Southern Alps; (2) eastward escape and extension
		of the Eastern Alps; (3) extensional collapse in the Pannonian basin
		area; (4) formation of broad wrench fault systems along strike in the
		Dinarides and Southern Carpathians, and the Western Carpathians with
		dextral and sinistral shear, respectively; (5) compression and
		accretion of the external thrust and fold belt in the Eastern
		Carpathians. These kinematic patterns are thought to be interrelated
		and all are manifestations of the late-stage evolution of an
		overthickened orogenic wedge.
		In order to arrive at a better understanding of the mechanism of
		extension, which formed the Pannonian basin, deep crustal seismic
		profiles, hydrocarbon exploration reflection lines and borehole data
		have been analyzed in the Little Hungarian Plain. This plain represents
		the transition zone between the Alps and the Pannonian lowlands, and
		the results are illustrated by eight interpreted cross-sections. One
		result of regional importance is the clear recognition that the
		Transdanubian Central Range at the southeastern flank of the Little
		Hungarian Plain is composed of Alpine (pre-Senonian) thrust sheets.
		This finding marks the end of a century of debate: the allochthony of
		the substrata of the Pannonian basin can be now considered proven.
		Another result of more general interest is that these cross-sections
		document the mode of lithospheric extension. Preexisting compressional
		detachment planes reactivate as low-angle normal faults and lead to
		tectonic unroofing of deeply buried metamorphic terranes characterized
		by ductile flow along subhorizontal lineation.},
	year = {1993},
	eissn = {1879-3266},
	pages = {333-357}
}

@article{MTMT:1155104,
	title = {The Itinerary of the Transdanubian Central Range: An assessment of relevant paleomagnetic observations.},
	url = {https://m2.mtmt.hu/api/publication/1155104},
	author = {Márton Péterné Szalay, Emőke},
	journal-iso = {ACTA GEOL HUNG},
	journal = {ACTA GEOLOGICA HUNGARICA: A QUARTERLY OF THE HUNGARIAN ACADEMY OF SCIENCES},
	volume = {37},
	unique-id = {1155104},
	issn = {0236-5278},
	year = {1993},
	pages = {135-151},
	orcid-numbers = {Márton Péterné Szalay, Emőke/0000-0002-2135-8867}
}

@article{MTMT:21017,
	title = {Jurassic microplate movements and brachiopod migrations in the western part of the Tethys},
	url = {https://m2.mtmt.hu/api/publication/21017},
	author = {Vörös, Attila},
	doi = {10.1016/0031-0182(93)90037-J},
	journal-iso = {PALAEOGEOGR PALAEOCL},
	journal = {PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY},
	volume = {100},
	unique-id = {21017},
	issn = {0031-0182},
	abstract = {The paleobiogeography of the Jurassic brachiopods of the Alpine-Carpathian region and adjacent areas is discussed on the basis of the distribution of ''distinctive taxa''. The Jurassic microplates of the western part of Tethys and the present-day ''terranes'' of the Alpine-Carpathian region are outlined and their relationships are discussed. The migration possibilities of the brachiopods in the Jurassic Tethys were controlled mainly by plate/microplate movements and by changes in the oceanic current system.
		
		The Mediterranean microcontinent, isolated from the European and African shelves by oceanic/deep-sea belts, was the homeland of the Mediterranean brachiopod province. In the course of the Jurassic, the Mediterranean microcontinent moved, as part of the African plate, away from Europe, the widening Alboran-Ligurian-Penninic oceanic belt became a barrier preventing migration of brachiopods. By the end of the Middle Jurassic the Tisza microplate detached from Europe and formed a ''stepping stone'' for brachiopod dispersal. At about the same time, the ''Hesperian Strait'' opened between the basins of the Tethys and the Central Atlantic. The opening of this strait resulted in a reorganization of the Tethyan current system. The westward flowing equatorial currents which made a turn in the western corner of Tethys in the first half of the Mesozoic, now ran to the west through the Hesperian Strait via the Central Atlantic to the Pacific. This change produced a new pattern in brachiopod distribution: the Mediterranean fauna successfully invaded the European shelf, at the same time the Mediterranean province became impoverished.},
	year = {1993},
	eissn = {1872-616X},
	pages = {125-145}
}

@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:1368439,
	title = {GRAVITY-FLOW DOMINATED SEDIMENTATION ON THE BUDA PALEOSLOPE (HUNGARY) - RECORD OF LATE EOCENE CONTINENTAL ESCAPE OF THE BAKONY UNIT},
	url = {https://m2.mtmt.hu/api/publication/1368439},
	author = {Fodor, László and MAGYARI, A and Kázmér, Miklós and FOGARASI, A},
	doi = {10.1007/BF01791386},
	journal-iso = {GEOL RUNDSCH},
	journal = {GEOLOGISCHE RUNDSCHAU},
	volume = {81},
	unique-id = {1368439},
	issn = {0016-7835},
	year = {1992},
	pages = {695-716},
	orcid-numbers = {Kázmér, Miklós/0000-0003-1092-1316}
}

@article{MTMT:21057549,
	title = {Paleomagnetic investigations on late Cretaceous-Cenozoic sediments from the NW part of the Pannonian Basin.},
	url = {https://m2.mtmt.hu/api/publication/21057549},
	author = {Márton Péterné Szalay, Emőke and Pagác, P and Túnyi, I},
	journal-iso = {GEOL CARPATH},
	journal = {GEOLOGICA CARPATHICA},
	volume = {43},
	unique-id = {21057549},
	issn = {1335-0552},
	year = {1992},
	eissn = {1336-8052},
	pages = {363-368},
	orcid-numbers = {Márton Péterné Szalay, Emőke/0000-0002-2135-8867}
}

@article{MTMT:1855796,
	title = {REVIEW OF NEOGENE AND QUATERNARY VOLCANISM OF THE CARPATHIAN PANNONIAN REGION},
	url = {https://m2.mtmt.hu/api/publication/1855796},
	author = {Szabó, Csaba and Harangi, Szabolcs and Csontos, László},
	doi = {10.1016/0040-1951(92)90347-9},
	journal-iso = {TECTONOPHYSICS},
	journal = {TECTONOPHYSICS},
	volume = {208},
	unique-id = {1855796},
	issn = {0040-1951},
	year = {1992},
	eissn = {1879-3266},
	pages = {243-256},
	orcid-numbers = {Szabó, Csaba/0000-0002-1580-6344; Harangi, Szabolcs/0000-0003-2372-4581}
}

@article{MTMT:1255444,
	title = {Styles of extension in the Pannonian Basin.},
	url = {https://m2.mtmt.hu/api/publication/1255444},
	author = {Tari, Gábor and Horváth, Ferenc and RUMPLER, J},
	doi = {10.1016/0040-1951(92)90345-7},
	journal-iso = {TECTONOPHYSICS},
	journal = {TECTONOPHYSICS},
	volume = {208},
	unique-id = {1255444},
	issn = {0040-1951},
	abstract = {Structural interpretation of reflection seismic profiles reveals distinct modes of upper crustal extension in the Pannonian Basin. While some subbasins in the Pannonian Basin complex show little extension (planar rotational normal faults), others are characterized by large magnitude of extension (detachment faults, metamorphic core complexes). Gravitational collapse of the Intra-Carpathian domain, combined with subduction zone roll-back is thought to be the driving mechanism of the Neogene back-arc extension.
		
		The very heterogeneously distributed extension is accommodated by transfer faults, which bound regions characterized by different polarity, direction, or amount of extension. In cross section these transfer faults are characterized by flower structures, typical for strike-slip faults.
		
		Seismic stratigraphic interpretations indicate that the non-marine post-rift sedimentary fill of the Pannonian Basin can be described in terms of sequence stratigraphy. The exceptionally good seismic sequence resolution allows recognition of third-order and also fourth-order depositional sequences, which may reflect the interplay of tectonics and eustasy, and Milankovitch scale climatic variations, respectively.},
	year = {1992},
	eissn = {1879-3266},
	pages = {203-219}
}

@article{MTMT:1383045,
	title = {PERMIAN CIRCUMPACIFIC DEEP-WATER FAUNAS FROM THE WESTERN TETHYS (SICILY, ITALY) - NEW EVIDENCES FOR THE POSITION OF THE PERMIAN TETHYS},
	url = {https://m2.mtmt.hu/api/publication/1383045},
	author = {CATALANO, R and DISTEFANO, P and Kozur, Heinz},
	doi = {10.1016/0031-0182(91)90131-A},
	journal-iso = {PALAEOGEOGR PALAEOCL},
	journal = {PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY},
	volume = {87},
	unique-id = {1383045},
	issn = {0031-0182},
	abstract = {Circumpacific deep-water faunas, characterized mainly by radiolarians, paleopsychrospheric ostracods and conodonts, were found in the early, middle and late Permian deposits pertaining to the Sicanian paleogeographic domain of western Sicily, near the western end of the Eurasiatic Tethys. Similar Permian deep-water faunas are known from the Phyllite Unit of Crete and from Oman in the latter area partly above oceanic crust. All these occurrences indicate the presence of a late Paleozoic Tethys ocean immediately north of Gondwana.},
	keywords = {history},
	year = {1991},
	eissn = {1872-616X},
	pages = {75-108}
}

@article{MTMT:1114237,
	title = {Very low- and low-grade metamorphic rocks in the pre-Tertiary basement of the Drave Basin, SW-Hungary: mineral assemblages, illite crystallinity, b0 data, and problems of geological correlation},
	url = {https://m2.mtmt.hu/api/publication/1114237},
	author = {Árkai, Péter},
	journal-iso = {ACTA GEOL HUNG},
	journal = {ACTA GEOLOGICA HUNGARICA: A QUARTERLY OF THE HUNGARIAN ACADEMY OF SCIENCES},
	volume = {33},
	unique-id = {1114237},
	issn = {0236-5278},
	year = {1990},
	pages = {43-67}
}

@article{MTMT:1072504,
	title = {The Lower Sinemurian (Jurassic) brachiopod fauna of the Lókút Hill (Bakony Mountains, Hungary). Preliminary results.},
	url = {https://m2.mtmt.hu/api/publication/1072504},
	author = {Dulai, Alfréd},
	journal-iso = {ANNLS HIST-NAT MUS NAT HUNG},
	journal = {ANNALES HISTORICO-NATURALES MUSEI NATIONALIS HUNGARICI},
	volume = {82},
	unique-id = {1072504},
	issn = {0521-4726},
	year = {1990},
	eissn = {2786-1368},
	pages = {25-37}
}

@article{MTMT:1154968,
	title = {Kinematics of the principal tectonic units of Hungary from paleomagnetic observations.},
	url = {https://m2.mtmt.hu/api/publication/1154968},
	author = {Márton Péterné Szalay, Emőke},
	journal-iso = {ACTA GEOD GEOPHYS MONTAN HUNG},
	journal = {ACTA GEODAETICA GEOPHYSICA ET MONTANISTICA HUNGARICA},
	volume = {25},
	unique-id = {1154968},
	issn = {0236-5758},
	year = {1990},
	pages = {387-397},
	orcid-numbers = {Márton Péterné Szalay, Emőke/0000-0002-2135-8867}
}

@article{MTMT:2222072,
	title = {Középső liász bivalviák paleobiogeográfiai értékelése az alp-kárpáti régióban.},
	url = {https://m2.mtmt.hu/api/publication/2222072},
	author = {Szente, István},
	journal-iso = {ÁLTALÁNOS FÖLDTANI SZEMLE},
	journal = {ÁLTALÁNOS FÖLDTANI SZEMLE},
	volume = {25},
	unique-id = {2222072},
	issn = {0133-6339},
	year = {1990},
	pages = {223-229}
}

@inbook{MTMT:1902908,
	title = {Submarine fan-channel conglomerate of Lower Cretaceous, Gerecse Mts., Hungary},
	url = {https://m2.mtmt.hu/api/publication/1902908},
	author = {Sztanó, Orsolya},
	booktitle = {Neues Jahrbuch für Geologie und Paläontologie},
	unique-id = {1902908},
	year = {1990},
	pages = {431-446},
	orcid-numbers = {Sztanó, Orsolya/0000-0003-0786-3653}
}

@article{MTMT:1021646,
	title = {Triassic evolution of the Periadriatic margin in Hungary},
	url = {https://m2.mtmt.hu/api/publication/1021646},
	author = {Vörös, Attila and Horváth, Ferenc and Galácz, András},
	journal-iso = {BOLL SOC GEOL ITAL},
	journal = {BOLLETTINO DELLA SOCIETA GEOLOGICA ITALIANA},
	volume = {109},
	unique-id = {1021646},
	issn = {0037-8763},
	year = {1990},
	pages = {73-81}
}

@article{MTMT:1114238,
	title = {The age of metamorphism of the East Alpine-type basement, Little Plain, W-Hungary: K-Ar dating of K-white micas from very low- and low-grade metamorphic rocks},
	url = {https://m2.mtmt.hu/api/publication/1114238},
	author = {Árkai, Péter and Balogh, Kadosa},
	journal-iso = {ACTA GEOL HUNG},
	journal = {ACTA GEOLOGICA HUNGARICA: A QUARTERLY OF THE HUNGARIAN ACADEMY OF SCIENCES},
	volume = {32},
	unique-id = {1114238},
	issn = {0236-5278},
	year = {1989},
	pages = {131-147}
}

@inbook{MTMT:1834233,
	title = {Triassic and Jurassic oceanic/paraoceanic belts in the Carpathian-Pannonian region and its surroundings.},
	url = {https://m2.mtmt.hu/api/publication/1834233},
	author = {Kázmér, Miklós and Kovács, Sándor},
	booktitle = {Tectonic Evolution of the Tethyan Region.},
	unique-id = {1834233},
	year = {1989},
	pages = {77-92},
	orcid-numbers = {Kázmér, Miklós/0000-0003-1092-1316}
}

@article{MTMT:1054085,
	title = {A compilation of palaeomagnetic results from Hungary},
	url = {https://m2.mtmt.hu/api/publication/1054085},
	author = {Márton Péterné Szalay, Emőke and Márton, Péter},
	journal-iso = {GEOFIZIKAI KÖZLEMÉNYEK},
	journal = {GEOFIZIKAI KÖZLEMÉNYEK - GEOPHYSICAL TRANSACTIONS},
	volume = {35},
	unique-id = {1054085},
	issn = {0016-7177},
	year = {1989},
	pages = {117-133},
	orcid-numbers = {Márton Péterné Szalay, Emőke/0000-0002-2135-8867}
}

@article{MTMT:1019301,
	title = {Triassic key sections in the Mid-Transdanubian (Igal) structural zone},
	url = {https://m2.mtmt.hu/api/publication/1019301},
	author = {Haas, János and E, Rálisch-Felgenhauer and A, Oravecz-Scheffer and A, Bérczi-Makk and E, Nagy},
	journal-iso = {ACTA GEOL HUNG},
	journal = {ACTA GEOLOGICA HUNGARICA: A QUARTERLY OF THE HUNGARIAN ACADEMY OF SCIENCES},
	volume = {31},
	unique-id = {1019301},
	issn = {0236-5278},
	year = {1988},
	pages = {3-18},
	orcid-numbers = {Haas, János/0000-0003-0929-8889}
}

@article{MTMT:1311204,
	title = {Az Aggtelek-Rudabányai-hegység triász formációi [Triassic formations of the Aggtelek-Rudabánya Mts.]},
	url = {https://m2.mtmt.hu/api/publication/1311204},
	author = {Kovács, S and Less, György and Piros, Olga and Róth, L},
	journal-iso = {M ÁLL FÖLDT INT JELENT},
	journal = {MAGYAR ÁLLAMI FÖLDTANI INTÉZET ÉVI JELENTÉSE},
	volume = {1986},
	unique-id = {1311204},
	issn = {0368-9751},
	year = {1988},
	pages = {19-43}
}

@misc{MTMT:1996087,
	title = {Az Aggtelek–Rudabányai-hegység fedetlen földtani térképe M = 1: 25.000},
	url = {https://m2.mtmt.hu/api/publication/1996087},
	author = {Less, Gy and Grill, J and Szentpétery, Ildikó and Róth, L and Gyuricza, György},
	editor = {Less, Gy and Grill, J and Szentpétery, Ildikó},
	unique-id = {1996087},
	year = {1988}
}

@article{MTMT:1019273,
	title = {Position of the Transdanubian Central Range structural unit in the Alpine evolution phase},
	url = {https://m2.mtmt.hu/api/publication/1019273},
	author = {Haas, János},
	journal-iso = {ACTA GEOL HUNG},
	journal = {ACTA GEOLOGICA HUNGARICA: A QUARTERLY OF THE HUNGARIAN ACADEMY OF SCIENCES},
	volume = {30},
	unique-id = {1019273},
	issn = {0236-5278},
	year = {1987},
	pages = {243-256},
	orcid-numbers = {Haas, János/0000-0003-0929-8889}
}

@article{MTMT:1255424,
	title = {New geophysical data: evidence for the allochthony of the Transdanubian Central Range},
	url = {https://m2.mtmt.hu/api/publication/1255424},
	author = {Horváth, Ferenc and Ádám, Antal and Stanley, WS},
	journal-iso = {REND SOC GEOL ITAL},
	journal = {RENDICONTI DELLA SOCIETA GEOLOGICA ITALIANA},
	volume = {9},
	unique-id = {1255424},
	issn = {0392-3037},
	year = {1987},
	pages = {123-130}
}

@article{MTMT:1154348,
	title = {Paleomagnetism and tectonics in the Mediterranean region.},
	url = {https://m2.mtmt.hu/api/publication/1154348},
	author = {Márton Péterné Szalay, Emőke},
	doi = {10.1016/0264-3707(87)90062-7},
	journal-iso = {J GEODYN},
	journal = {JOURNAL OF GEODYNAMICS},
	volume = {7},
	unique-id = {1154348},
	issn = {0264-3707},
	year = {1987},
	pages = {33-57},
	orcid-numbers = {Márton Péterné Szalay, Emőke/0000-0002-2135-8867}
}

@article{MTMT:1019111,
	title = {Az MK-1/82. geofizikai alapvonal Dabrony-Devecser közti szakaszának földtani értelmezése},
	url = {https://m2.mtmt.hu/api/publication/1019111},
	author = {Ádám, O and Ráner, G and Haas, János},
	journal-iso = {MAGYAR ÁLLAMI EÖTVÖS LORÁND GEOFIZIKAI INT ÉVI JELENTÉSE},
	journal = {MAGYAR ÁLLAMI EÖTVÖS LORÁND GEOFIZIKAI INTÉZET ÉVI JELENTÉSE = ANNUAL REPORT OF THE EOTVOS LORAND GEOPHYSICAL INSTITUTE OF HUNGARY},
	volume = {1983},
	unique-id = {1019111},
	issn = {0524-8655},
	year = {1985},
	pages = {117-121},
	orcid-numbers = {Haas, János/0000-0003-0929-8889}
}

@article{MTMT:1021617,
	title = {Jurassic of Hungary: a review},
	url = {https://m2.mtmt.hu/api/publication/1021617},
	author = {Galácz, András},
	journal-iso = {ACTA GEOL HUNG},
	journal = {ACTA GEOLOGICA HUNGARICA: A QUARTERLY OF THE HUNGARIAN ACADEMY OF SCIENCES},
	volume = {27},
	unique-id = {1021617},
	issn = {0236-5278},
	year = {1985},
	pages = {359-377}
}

@article{MTMT:1021618,
	title = {Sedimentary and structural evolution of the Bakony Mountains (Transdanubian Central Range, Hungary): paleogeographic implications},
	url = {https://m2.mtmt.hu/api/publication/1021618},
	author = {Galácz, András and Horváth, Ferenc and Vörös, Attila},
	journal-iso = {ACTA GEOL HUNG},
	journal = {ACTA GEOLOGICA HUNGARICA: A QUARTERLY OF THE HUNGARIAN ACADEMY OF SCIENCES},
	volume = {28},
	unique-id = {1021618},
	issn = {0236-5278},
	year = {1985},
	pages = {85-100}
}

@article{MTMT:1834167,
	title = {Permian-Paleogene paleogeography along the eastern part of the Insubric-Periadriatic lineament system: Evidence for continental escape of the Bakony-Drauzug unit.},
	url = {https://m2.mtmt.hu/api/publication/1834167},
	author = {Kázmér, Miklós and KOVÁCS, Sándor},
	journal-iso = {ACTA GEOL HUNG},
	journal = {ACTA GEOLOGICA HUNGARICA: A QUARTERLY OF THE HUNGARIAN ACADEMY OF SCIENCES},
	volume = {28},
	unique-id = {1834167},
	issn = {0236-5278},
	year = {1985},
	pages = {71-84},
	orcid-numbers = {Kázmér, Miklós/0000-0003-1092-1316}
}

@article{MTMT:1019097,
	title = {A szenon nekézsenyi konglomerátum formáció sztratotípus szelvényének szedimentológiai és tektonikai vizsgálata},
	url = {https://m2.mtmt.hu/api/publication/1019097},
	author = {Brezsnyánszky, Károly and Haas, János},
	journal-iso = {FÖLDTANI KÖZLÖNY},
	journal = {FÖLDTANI KÖZLÖNY},
	volume = {114},
	unique-id = {1019097},
	issn = {0015-542X},
	year = {1984},
	eissn = {2559-902X},
	pages = {81-100},
	orcid-numbers = {Haas, János/0000-0003-0929-8889}
}

@article{MTMT:1114268,
	title = {Very low- and low-grade Alpine regional metamorphism of the paleozoic and mesozoic formations of the Bükkium, NE-Hungary},
	url = {https://m2.mtmt.hu/api/publication/1114268},
	author = {Árkai, Péter},
	journal-iso = {ACTA GEOL HUNG},
	journal = {ACTA GEOLOGICA HUNGARICA: A QUARTERLY OF THE HUNGARIAN ACADEMY OF SCIENCES},
	volume = {26},
	unique-id = {1114268},
	issn = {0236-5278},
	year = {1983},
	pages = {83-101}
}

@article{MTMT:1255403,
	title = {Mechanism for the formation of the intra-Carpathian basins: a review},
	url = {https://m2.mtmt.hu/api/publication/1255403},
	author = {Horváth, Ferenc and Royden, L},
	journal-iso = {EARTH EVOL SCI},
	journal = {EARTH EVOLUTION SCIENCES},
	volume = {1},
	unique-id = {1255403},
	issn = {1881-8463},
	year = {1981},
	pages = {307-316}
}

@article{MTMT:1041921,
	title = {A Dunántúli-középhegység és a Villányi-hegység mezozoós paleopólusainak eltérésérõl},
	url = {https://m2.mtmt.hu/api/publication/1041921},
	author = {Márton Péterné Szalay, Emőke and Márton, Péter},
	journal-iso = {MAGYAR GEOFIZIKA},
	journal = {MAGYAR GEOFIZIKA},
	volume = {19},
	unique-id = {1041921},
	issn = {0025-0120},
	year = {1978},
	eissn = {2677-1497},
	pages = {129-136},
	orcid-numbers = {Márton Péterné Szalay, Emőke/0000-0002-2135-8867}
}

@article{MTMT:20954,
	title = {Provinciality of the Mediterranean Lower Jurassic brachiopod fauna: causes and plate tectonic implications},
	url = {https://m2.mtmt.hu/api/publication/20954},
	author = {Vörös, Attila},
	doi = {10.1016/0031-0182(77)90002-5},
	journal-iso = {PALAEOGEOGR PALAEOCL},
	journal = {PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY},
	volume = {21},
	unique-id = {20954},
	issn = {0031-0182},
	year = {1977},
	eissn = {1872-616X},
	pages = {1-16}
}

@article{MTMT:1255393,
	title = {AFRICAN-ADRIATIC PROMONTORY AS A PALEO-GEOGRAPHICAL PREMISE FOR ALPINE OROGENY AND PLATE MOVEMENTS IN CARPATHO-BALKAN REGION},
	url = {https://m2.mtmt.hu/api/publication/1255393},
	author = {CHANNELL, JET and Horváth, Ferenc},
	doi = {10.1016/0040-1951(76)90030-5},
	journal-iso = {TECTONOPHYSICS},
	journal = {TECTONOPHYSICS},
	volume = {35},
	unique-id = {1255393},
	issn = {0040-1951},
	year = {1976},
	eissn = {1879-3266},
	pages = {71-101}
}