@article{MTMT:2783510,
	title = {Statistical characterization of brittle and semi-brittle fault rocks: a clast geometry approach},
	url = {https://m2.mtmt.hu/api/publication/2783510},
	author = {Molnár, László and M. Tóth, Tivadar and Schubert, Félix},
	doi = {10.1007/s40328-014-0067-3},
	journal-iso = {ACTA GEOD GEOPHYS},
	journal = {ACTA GEODAETICA ET GEOPHYSICA},
	volume = {49},
	unique-id = {2783510},
	issn = {2213-5812},
	year = {2014},
	eissn = {2213-5820},
	pages = {527-550},
	orcid-numbers = {M. Tóth, Tivadar/0000-0003-1012-1095; Schubert, Félix/0000-0001-8647-5354}
}

@inbook{MTMT:1382869,
	title = {Az aljzati kristályos hátak szerepe az Alföld fluidum áramlási és hőtranszport folyamataiban},
	url = {https://m2.mtmt.hu/api/publication/1382869},
	author = {Vass, I and M. Tóth, Tivadar and Szanyi, János and Kovács, Balázs},
	booktitle = {Magmás és metamorf képződmények a Tiszai Egységben},
	unique-id = {1382869},
	year = {2009},
	pages = {325-339},
	orcid-numbers = {M. Tóth, Tivadar/0000-0003-1012-1095; Szanyi, János/0000-0002-8053-6360}
}

@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:2176402,
	title = {Formation and deformation of the Pannonian Basin: Constraints from observational data},
	url = {https://m2.mtmt.hu/api/publication/2176402},
	isbn = {1862392129},
	author = {Horváth, Ferenc and Bada, G and Szafián, P and Tari, Gábor and Ádám, A and Cloetingh, S},
	doi = {10.1144/GSL.MEM.2006.032.01.11},
	journal-iso = {MEM GEOL SOC LOND},
	journal = {MEMOIRS OF THE GEOLOGICAL SOCIETY OF LONDON},
	volume = {32},
	unique-id = {2176402},
	issn = {0435-4052},
	abstract = {The past decade has witnessed spectacular progress in the collection of observational data and their interpretation in the Pannonian Basin and the surrounding Alpine, Carpathian and Dinaric mountain belts. A major driving force behind this progress was the PANCARDI project of the EUROPROBE programme. The paper reviews tectonic processes, structural styles, stratigraphic records and geochemical data for volcanic rocks. Structural and seismic sections of different scales, seismic tomography and magnetotelluric, gravity and geothermal data are also used to determine the deformational styles, and to compile new crustal and lithospheric thickness maps of the Pannonian Basin and the surrounding fold-and-thrust belts. The Pannonian Basin is superimposed on former Alpine terranes. Its formation is a result of extensional collapse of the overthickened Alpine orogenic wedge during orogen-parallel extrusion towards a 'free boundary' offered by the roll-back of the subducting Carpathian slab, As a conclusion, continental collision and back-arc basin evolution is discussed as a single, complex dynamic process, with minimization of the potential and deformational energy as the driving principle. © The Geological Society of London 2006.},
	keywords = {Europe; Eurasia; extrusion; SUBDUCTION; Pannonian Basin; continental collision; orogeny; basin evolution; Formation mechanism; deformation mechanism; fold and thrust belt; backarc basin; tectonic wedge},
	year = {2006},
	eissn = {2041-4722},
	pages = {191-206}
}

@article{MTMT:1129815,
	title = {Conceptual fracture network model of the crystalline basement of the Szeghalom Dome (Pannonian Basin, SE Hungary)},
	url = {https://m2.mtmt.hu/api/publication/1129815},
	author = {M. Tóth, Tivadar and Szűcs, É and Schubert, Félix and Hollós, Cs},
	doi = {10.1556/AGeol.47.2004.1.2},
	journal-iso = {ACTA GEOL HUNG},
	journal = {ACTA GEOLOGICA HUNGARICA: A QUARTERLY OF THE HUNGARIAN ACADEMY OF SCIENCES},
	volume = {47},
	unique-id = {1129815},
	issn = {0236-5278},
	year = {2004},
	pages = {19-34},
	orcid-numbers = {M. Tóth, Tivadar/0000-0003-1012-1095; Schubert, Félix/0000-0001-8647-5354}
}

@article{MTMT:1129807,
	title = {Connected fluid evolution in fractured crystalline basement and overlying sediments, Pannonian Basin, SE Hungary},
	url = {https://m2.mtmt.hu/api/publication/1129807},
	author = {Juhász, A and M. Tóth, Tivadar and Ramseyer, K and Matter, A},
	doi = {10.1016/S0009-2541(01)00269-8},
	journal-iso = {CHEM GEOL},
	journal = {CHEMICAL GEOLOGY},
	volume = {182},
	unique-id = {1129807},
	issn = {0009-2541},
	year = {2002},
	eissn = {1872-6836},
	pages = {91-120},
	orcid-numbers = {M. Tóth, Tivadar/0000-0003-1012-1095}
}

@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: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:2899915,
	title = {The mid-Hungarian line: a zone of repeated tectonic inversions},
	url = {https://m2.mtmt.hu/api/publication/2899915},
	author = {Csontos, L and Nagymarosy, András},
	doi = {10.1016/S0040-1951(98)00163-2},
	journal-iso = {TECTONOPHYSICS},
	journal = {TECTONOPHYSICS},
	volume = {297},
	unique-id = {2899915},
	issn = {0040-1951},
	abstract = {The Mid-Hungarian line is a major tectonic feature of the Intra-Carpathian area separating two terranes of different origin and tectonic structure. Although this tectonic line was known from borehole records, it has not been described in seismic sections. The study presents interpreted seismic lines crossing the supposed trace of the Mid-Hungarian line. These seismic sections show north-dipping normal faults and thrust faults as well as cross-cutting young strike-slip faults. A complex tectonic history is deduced, including intra-Oligocene-Early Miocene thrusting, Middle Miocene extension, local Late Miocene inversion and Late Miocene-Pliocene normal faulting and left-lateral wrenching. In the light of our seismic study we think that the best candidate for the Mid-Hungarian line is a north-dipping detachment fault beneath large masses of Neogene volcanics. The auxiliary structures to the north seen on seismic sections suggest that it moved as a south-vergent thrust fault during the Palaeogene-Early Miocene which later was reactivated as a set of normal faults. The northern Alcapa unit overrode the southern Tisza-Dacia unit along this fault zone. The same relative positions are observed in the northern termination of the line. Other structures along the supposed trace of the line are north-dipping normal-or strike-slip faults which frequently were reactivated as smaller thrust faults during the late Neogene. Palaeogene-Early Miocene thrusting along the line might be the result of the opposite Tertiary rotations of the two major units, as suggested by palaeomagnetic measurements and earlier models. (C) 1998 Elsevier Science B.V. All rights reserved.},
	year = {1998},
	eissn = {1879-3266},
	pages = {51-71}
}

@article{MTMT:1441803,
	title = {Asthenospheric structure beneath a Neogene basin in southeast Hungary},
	url = {https://m2.mtmt.hu/api/publication/1441803},
	author = {Posgay, Károly and Bodoky, Tamás János and Hegedűs, Endre and Kovácsvölgyi, S and Lenkey, László and Szafián, P and Takács, Ernő and Csabafi, Róbert Imre and Varga, G},
	doi = {10.1016/0040-1951(95)00098-4},
	journal-iso = {TECTONOPHYSICS},
	journal = {TECTONOPHYSICS},
	volume = {252},
	unique-id = {1441803},
	issn = {0040-1951},
	year = {1995},
	eissn = {1879-3266},
	pages = {467-484},
	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}
}