@article{MTMT:31614407,
	title = {Lithologically controlled behaviour of the Dorozsma metamorphic hydrocarbon reservoir (Pannonian Basin, SE Hungary)},
	url = {https://m2.mtmt.hu/api/publication/31614407},
	author = {M. Tóth, Tivadar and Vargáné Tóth, I},
	doi = {10.1016/j.petrol.2020.107748},
	journal-iso = {J PETROL SCI ENG},
	journal = {JOURNAL OF PETROLEUM SCIENCE AND ENGINEERING},
	volume = {195},
	unique-id = {31614407},
	issn = {0920-4105},
	year = {2020},
	eissn = {1873-4715},
	orcid-numbers = {M. Tóth, Tivadar/0000-0003-1012-1095}
}

@article{MTMT:27569302,
	title = {Evolution of the arc-derived orthogneiss recorded in exotic xenoliths of the Koros Complex (Tisza Megaunit, SE Hungary)},
	url = {https://m2.mtmt.hu/api/publication/27569302},
	author = {M. Tóth, Tivadar and Schubert, Félix},
	doi = {10.3190/jgeosci.253},
	journal-iso = {J GEOSCI},
	journal = {JOURNAL OF GEOSCIENCES},
	volume = {63},
	unique-id = {27569302},
	issn = {1802-6222},
	year = {2018},
	eissn = {1803-1943},
	pages = {21-46},
	orcid-numbers = {M. Tóth, Tivadar/0000-0003-1012-1095; 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:2949635,
	title = {Structural controls on petroleum migration and entrapment within the faulted basement blocks of Szeghalom Dome (Pannonian Basin, SE Hungary)},
	url = {https://m2.mtmt.hu/api/publication/2949635},
	author = {Molnár, L and M. Tóth, Tivadar and Schubert, Félix},
	doi = {10.4154/gc.2015.19},
	journal-iso = {GEOL CROAT},
	journal = {GEOLOGIA CROATICA},
	volume = {68},
	unique-id = {2949635},
	issn = {1330-030X},
	year = {2015},
	eissn = {1333-4875},
	pages = {247-259},
	orcid-numbers = {M. Tóth, Tivadar/0000-0003-1012-1095; Schubert, Félix/0000-0001-8647-5354}
}

@article{MTMT:2474978,
	title = {Lithology identification using open-hole well-log data in the metamorphic Kiskunhalas-NE hydrocarbon reservoir, South Hungary},
	url = {https://m2.mtmt.hu/api/publication/2474978},
	author = {Fiser-Nagy, Ágnes and Varga-Tóth, I and M. Tóth, Tivadar},
	doi = {10.1007/s40328-013-0037-1},
	journal-iso = {ACTA GEOD GEOPHYS},
	journal = {ACTA GEODAETICA ET GEOPHYSICA},
	volume = {49},
	unique-id = {2474978},
	issn = {2213-5812},
	abstract = {in press},
	year = {2014},
	eissn = {2213-5820},
	pages = {57-78},
	orcid-numbers = {M. Tóth, Tivadar/0000-0003-1012-1095}
}

@article{MTMT:2190426,
	title = {Integrated core study of a fractured metamorphic HC-reservoir; Kiskunhalas-NE, Pannonian Basin},
	url = {https://m2.mtmt.hu/api/publication/2190426},
	author = {Fiser-Nagy, Ágnes and M. Tóth, Tivadar and Vásárhelyi, Balázs and Földes, Tamás},
	doi = {10.1007/s40328-012-0008-y},
	journal-iso = {ACTA GEOD GEOPHYS},
	journal = {ACTA GEODAETICA ET GEOPHYSICA},
	volume = {48},
	unique-id = {2190426},
	issn = {2213-5812},
	year = {2013},
	eissn = {2213-5820},
	pages = {53-75},
	orcid-numbers = {M. Tóth, Tivadar/0000-0003-1012-1095; Vásárhelyi, Balázs/0000-0002-0568-1031}
}

@article{MTMT:2011063,
	title = {Mafic enclaves in peraluminous Variscan granitoid in the Battonya Unit from Southeast Hungary},
	url = {https://m2.mtmt.hu/api/publication/2011063},
	author = {Buda, György and Pál-Molnár, Elemér and Koller, F},
	doi = {10.4154/GC.2012.15},
	journal-iso = {GEOL CROAT},
	journal = {GEOLOGIA CROATICA},
	volume = {65},
	unique-id = {2011063},
	issn = {1330-030X},
	keywords = {Hungary; igneous intrusion; magmatism; mafic rock; Mica; calc alkaline rock; biotite; Micas; muscovite; granitoid; Hercynian orogeny; AMPHIBOLE; hydrothermal alteration; Feldspar; T; P; SE Hungary; secondary muscovite; primary-; I/S-type; peraluminous granitoid; basic enclave; Variscan; Depth of intrusion; enclave},
	year = {2012},
	eissn = {1333-4875},
	pages = {243-253},
	orcid-numbers = {Pál-Molnár, Elemér/0000-0002-9606-0133}
}

@article{MTMT:1843346,
	title = {Petrology and tectonic evolution of the Kiskunhalas-NE fractured hydrocarbon reservoir, South Hungary},
	url = {https://m2.mtmt.hu/api/publication/1843346},
	author = {Fiser-Nagy, Ágnes and M. Tóth, Tivadar},
	doi = {10.1556/CEuGeol.55.2012.1.1},
	journal-iso = {CENT EUR GEOL},
	journal = {CENTRAL EUROPEAN GEOLOGY},
	volume = {55},
	unique-id = {1843346},
	issn = {1788-2281},
	year = {2012},
	eissn = {1789-3348},
	pages = {1-22},
	orcid-numbers = {M. Tóth, Tivadar/0000-0003-1012-1095}
}

@inbook{MTMT:1348928,
	title = {A polimetamorf aljzat geokronológiai viszonyai a Szeghalom és a Mezősas-Furta háton},
	url = {https://m2.mtmt.hu/api/publication/1348928},
	author = {Balogh, K and M. Tóth, Tivadar and Dunkl, István and Scherrer, N},
	booktitle = {Magmás és metamorf képződmények a Tiszai Egységben},
	unique-id = {1348928},
	year = {2009},
	pages = {147-160},
	orcid-numbers = {M. Tóth, Tivadar/0000-0003-1012-1095}
}

@inbook{MTMT:1382756,
	title = {A Jánoshalma eklogit petrológiája},
	url = {https://m2.mtmt.hu/api/publication/1382756},
	author = {Zachar, J and M. Tóth, Tivadar},
	booktitle = {Magmás és metamorf képződmények a Tiszai Egységben},
	unique-id = {1382756},
	year = {2009},
	pages = {117-144},
	orcid-numbers = {M. Tóth, Tivadar/0000-0003-1012-1095}
}

@article{MTMT:1348922,
	title = {A Szeghalom környéki metamorf aljzat kiemelkedés szerkezetfejlődése és felépítése kőzettani és szeizmikus adatok alapján [Structural evolution of the Szeghalom metamorphic dome on the basis of petrological and seismic data]},
	url = {https://m2.mtmt.hu/api/publication/1348922},
	author = {M. Tóth, Tivadar and Redlerné, Tátrai M and Kummer, I},
	journal-iso = {MAGYAR GEOFIZIKA},
	journal = {MAGYAR GEOFIZIKA},
	volume = {49},
	unique-id = {1348922},
	issn = {0025-0120},
	year = {2008},
	eissn = {2677-1497},
	pages = {143-151},
	orcid-numbers = {M. Tóth, Tivadar/0000-0003-1012-1095}
}

@mastersthesis{MTMT:30931322,
	title = {Repedezett, metamorf fluidumtárolók az Alföld aljazatában},
	url = {https://m2.mtmt.hu/api/publication/30931322},
	author = {M. Tóth, Tivadar},
	unique-id = {30931322},
	year = {2008},
	orcid-numbers = {M. Tóth, Tivadar/0000-0003-1012-1095}
}

@article{MTMT:1129827,
	title = {Fluid-inclusion evidence of petroleum migration through a buried metamorphic dome in the Pannonian Basin, Hungary},
	url = {https://m2.mtmt.hu/api/publication/1129827},
	author = {Schubert, Félix and Diamond, L W and M. Tóth, Tivadar},
	doi = {10.1016/j.chemgeo.2007.05.019},
	journal-iso = {CHEM GEOL},
	journal = {CHEMICAL GEOLOGY},
	volume = {244},
	unique-id = {1129827},
	issn = {0009-2541},
	year = {2007},
	eissn = {1872-6836},
	pages = {357-381},
	orcid-numbers = {Schubert, Félix/0000-0001-8647-5354; M. Tóth, Tivadar/0000-0003-1012-1095}
}

@article{MTMT:1129826,
	title = {Kyanite eclogite xenolith from the orthogneiss terrane of the Tisza Megaunit, Jánoshalma area, crystalline basement of southern Hungary},
	url = {https://m2.mtmt.hu/api/publication/1129826},
	author = {Zachar, J and M. Tóth, Tivadar and Janák, M},
	doi = {10.1016/j.lithos.2007.06.001},
	journal-iso = {LITHOS},
	journal = {LITHOS},
	volume = {99},
	unique-id = {1129826},
	issn = {0024-4937},
	year = {2007},
	eissn = {1872-6143},
	pages = {249-265},
	orcid-numbers = {M. Tóth, Tivadar/0000-0003-1012-1095}
}

@article{MTMT:1129819,
	title = {Petrology and deformation history of the metamorphic basement in the Mezősas-Furta crystalline high (SE Hungary)},
	url = {https://m2.mtmt.hu/api/publication/1129819},
	author = {M. Tóth, Tivadar and Zachar, J},
	doi = {10.1556/AGeol.49.2006.2.4},
	journal-iso = {ACTA GEOL HUNG},
	journal = {ACTA GEOLOGICA HUNGARICA: A QUARTERLY OF THE HUNGARIAN ACADEMY OF SCIENCES},
	volume = {49},
	unique-id = {1129819},
	issn = {0236-5278},
	year = {2006},
	pages = {165-188},
	orcid-numbers = {M. Tóth, Tivadar/0000-0003-1012-1095}
}

@article{MTMT:1132980,
	title = {Metamorphic petrology and geochemistry of the Sarkadkeresztúr Basement-High with special regard to orthogneiss (Tisza Mega-unit, SE Hungary)},
	url = {https://m2.mtmt.hu/api/publication/1132980},
	author = {Pál-Molnár, Elemér and Lelkes-Felvári, Gy and Batki, Anikó and Sassi, R},
	doi = {10.1556/AGeol.48.2005.4.3},
	journal-iso = {ACTA GEOL HUNG},
	journal = {ACTA GEOLOGICA HUNGARICA: A QUARTERLY OF THE HUNGARIAN ACADEMY OF SCIENCES},
	volume = {48},
	unique-id = {1132980},
	issn = {0236-5278},
	year = {2005},
	pages = {395-418},
	orcid-numbers = {Pál-Molnár, Elemér/0000-0002-9606-0133}
}

@article{MTMT:1129817,
	title = {Petrology of the metamorphic basement of the Tisza block at the Jánoshalma high, S Hungary},
	url = {https://m2.mtmt.hu/api/publication/1129817},
	author = {Zachar, J and M. Tóth, Tivadar},
	doi = {10.1556/AGeol.47.2004.4.3},
	journal-iso = {ACTA GEOL HUNG},
	journal = {ACTA GEOLOGICA HUNGARICA: A QUARTERLY OF THE HUNGARIAN ACADEMY OF SCIENCES},
	volume = {47},
	unique-id = {1129817},
	issn = {0236-5278},
	year = {2004},
	pages = {349-371},
	orcid-numbers = {M. Tóth, Tivadar/0000-0003-1012-1095}
}

@article{MTMT:1129812,
	title = {Az Alföld metamorf aljzatának exhumációja a Szeghalom-dóm területén: palinológiai bizonyítékok},
	url = {https://m2.mtmt.hu/api/publication/1129812},
	author = {M. Tóth, Tivadar and Kedves, M and Schubert, Félix},
	journal-iso = {FÖLDTANI KÖZLÖNY},
	journal = {FÖLDTANI KÖZLÖNY},
	volume = {133},
	unique-id = {1129812},
	issn = {0015-542X},
	year = {2003},
	eissn = {2559-902X},
	pages = {547-562},
	orcid-numbers = {M. Tóth, Tivadar/0000-0003-1012-1095; Schubert, Félix/0000-0001-8647-5354}
}

@article{MTMT:1129800,
	title = {Neogene exhumation of the Variscan Szeghalom dome, Pannonian Basin, E. Hungary},
	url = {https://m2.mtmt.hu/api/publication/1129800},
	author = {M. Tóth, Tivadar and Schubert, Félix and Zachar, J},
	doi = {10.1002/gj.861},
	journal-iso = {GEOL J},
	journal = {GEOLOGICAL JOURNAL},
	volume = {35},
	unique-id = {1129800},
	issn = {0072-1050},
	year = {2000},
	eissn = {1099-1034},
	pages = {265-284},
	orcid-numbers = {M. Tóth, Tivadar/0000-0003-1012-1095; Schubert, Félix/0000-0001-8647-5354}
}

@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: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}
}