@inbook{MTMT:1258208,
	title = {Compression during extension in the Pannonian Basin and its bearing on hydrocarbon exploration},
	url = {https://m2.mtmt.hu/api/publication/1258208},
	author = {Horváth, Ferenc and Csontos, L and Cloetingh, S and Gerner, P and Dövényi, Péter},
	booktitle = {Oil and Gas in Alpidic Thrustbelts and Basins of Central and Eastern Europe},
	unique-id = {1258208},
	year = {1996},
	pages = {105-107}
}

@article{MTMT:1890264,
	title = {What can stable isotopes say about salinity? An example from the late Miocene Pannonian Lake},
	url = {https://m2.mtmt.hu/api/publication/1890264},
	author = {Matyas, J and Burns, SJ and Muller, P and Magyar, Imre},
	doi = {10.2307/3515114},
	journal-iso = {PALAIOS},
	journal = {PALAIOS},
	volume = {11},
	unique-id = {1890264},
	issn = {0883-1351},
	abstract = {The mid-to late Miocene ''Pannonian Lake'' was a primarily closed, saline lake which during its lifetime underwent a series of rapid salinity changes associated with faunal extinctions/radiations. The first two of these, at the Badenian/Sarmatian and Sarmatian/Pannonian boundaries signify the transition from a marine basin to a brackish lake and are marked by major faunal changes. The isotopic composition of molluscs from the lake, however, does not undergo major changes. The third transition, at the end of the Pannonian. and into the Pontian, is also marked by major faunal changes, thought initially to reflect further freshening of the lake. Both carbon, and oxygen isotope ratios of lake molluscs decrease by 4 to 6 parts per thousand at this transition. A consideration of salinity and oxygen. isotope mass balances for a closed or nearly-closed lake shows that major changes in salinity accompany relatively minor changes in water balance and isotopic composition. This result explains why the oxygen. isotope ratio of lake waters did not change during the initial freshening of the lake and suggests that the major isotopic changes observed later are not directly related to changes in the lake water balance which caused the salinity changes. The isotopic variations were driven mainly by other climatic factors, most likely changes in humidity and isotopic composition of inflow.},
	keywords = {CARBON; OXYGEN},
	year = {1996},
	eissn = {1938-5323},
	pages = {31-39}
}

@article{MTMT:1255453,
	title = {PHASES OF COMPRESSION DURING THE EVOLUTION OF THE PANNONIAN BASIN AND},
	url = {https://m2.mtmt.hu/api/publication/1255453},
	author = {Horváth, Ferenc},
	doi = {10.1016/0264-8172(95)98851-U},
	journal-iso = {MAR PETROL GEOL},
	journal = {MARINE AND PETROLEUM GEOLOGY},
	volume = {12},
	unique-id = {1255453},
	issn = {0264-8172},
	abstract = {Progress in understanding the structural evolution of the Pannonian
		Basin is reported. This has been driven by the application of seismic
		stratigraphy constrained by magnetostratigraphic data and the recent
		release of a great amount of hydrocarbon exploration data. This has led
		to a redefinition and better understanding of the syn-rift period and
		style of rifting. In addition, a complex structural evolution history
		during the post-rift phase has been recognized. Two compressive events
		are defined: one in the early stage and another in the late stage of
		evolution. The importance of these findings for hydrocarbon exploration
		includes an improved knowledge of the timing of trap formations and a
		possible explanation for remarkably variable reservoir pressures in
		pools of the Great Hungarian Plain.},
	year = {1995},
	eissn = {1873-4073},
	pages = {837-844}
}

@article{MTMT:2947503,
	title = {Hydraulic continuity in large sedimentary basins},
	url = {https://m2.mtmt.hu/api/publication/2947503},
	author = {Tóth, József},
	journal-iso = {HYDROGEOL J},
	journal = {HYDROGEOLOGY JOURNAL},
	volume = {3},
	unique-id = {2947503},
	issn = {1431-2174},
	year = {1995},
	eissn = {1435-0157},
	pages = {4-16}
}

@article{MTMT:22049448,
	title = {Paleogene retroarc flexural basin beneath the Neogene Pannonian Basin: A geodynamic model},
	url = {https://m2.mtmt.hu/api/publication/22049448},
	author = {Tari, Gábor and Báldi, T and Báldi-Beke, M},
	doi = {10.1016/0040-1951(93)90131-3},
	journal-iso = {TECTONOPHYSICS},
	journal = {TECTONOPHYSICS},
	volume = {226},
	unique-id = {22049448},
	issn = {0040-1951},
	year = {1993},
	eissn = {1879-3266},
	pages = {433-455}
}

@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:1129785,
	title = {Origin of some minerals from the crystalline basement of Szeghalom, Eastern Hungary},
	url = {https://m2.mtmt.hu/api/publication/1129785},
	author = {M. Tóth, Tivadar},
	journal-iso = {ACTA MINERAL PETROGR},
	journal = {ACTA MINERALOGICA PETROGRAPHICA},
	volume = {32},
	unique-id = {1129785},
	issn = {0365-8066},
	year = {1991},
	pages = {59-63},
	orcid-numbers = {M. Tóth, Tivadar/0000-0003-1012-1095}
}

@inbook{MTMT:1256140,
	title = {Subsidence; thermal; maturation history of the Great Hungarian Plain},
	url = {https://m2.mtmt.hu/api/publication/1256140},
	author = {Horváth, Ferenc and Dovenyi, P and Szalay, A and Royden, LH},
	booktitle = {The Pannonian Basin: A Study in Basin Evolution/Book and Maps},
	unique-id = {1256140},
	year = {1988},
	pages = {355-372}
}

@article{MTMT:1255411,
	title = {EVOLUTION OF THE PANNONIAN BASIN SYSTEM .1. TECTONICS},
	url = {https://m2.mtmt.hu/api/publication/1255411},
	author = {ROYDEN, L and Horváth, Ferenc and RUMPLER, J},
	doi = {10.1029/TC002i001p00063},
	journal-iso = {TECTONICS},
	journal = {TECTONICS},
	volume = {2},
	unique-id = {1255411},
	issn = {0278-7407},
	year = {1983},
	eissn = {1944-9194},
	pages = {63-90}
}

@article{MTMT:2947223,
	title = {A theoretical analysis of groundwater flow in small drainage basins},
	url = {https://m2.mtmt.hu/api/publication/2947223},
	author = {Tóth, József},
	journal-iso = {J GEOPHYS RES},
	journal = {JOURNAL OF GEOPHYSICAL RESEARCH},
	volume = {68},
	unique-id = {2947223},
	issn = {0148-0227},
	year = {1963},
	eissn = {2156-2202},
	pages = {4795-4812}
}