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

@article{MTMT:3385746,
	title = {„Oázis a sivatagban” — különösen gazdag ősmaradvány-együttes a fosszíliaszegény üllési Szegedi Dolomitból},
	url = {https://m2.mtmt.hu/api/publication/3385746},
	author = {Szurominé, Korecz Andrea and Garaguly, István and Szente, István and Raucsikné Varga, Andrea Beáta and Raucsik, Béla},
	doi = {10.23928/foldt.kozl.2018.148.2.119},
	journal-iso = {FÖLDTANI KÖZLÖNY},
	journal = {FÖLDTANI KÖZLÖNY},
	volume = {148},
	unique-id = {3385746},
	issn = {0015-542X},
	year = {2018},
	eissn = {2559-902X},
	pages = {119-124},
	orcid-numbers = {Garaguly, István/0000-0002-2802-0738; Raucsikné Varga, Andrea Beáta/0000-0002-8673-1482; Raucsik, Béla/0000-0002-1951-5974}
}

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

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

@article{MTMT:3097539,
	title = {The link between tectonics and sedimentation in back-arc basins: New genetic constraints from the analysis of the Pannonian Basin},
	url = {https://m2.mtmt.hu/api/publication/3097539},
	author = {Balázs, Attila and Matenco, L and Magyar, Imre and Horváth, Ferenc and Cloetingh, S},
	doi = {10.1002/2015TC004109},
	journal-iso = {TECTONICS},
	journal = {TECTONICS},
	volume = {35},
	unique-id = {3097539},
	issn = {0278-7407},
	abstract = {The architecture of sedimentary basins reflects the relationship between accommodation space and sediment supply, their rates and localization being variable during basin evolution. The mechanisms driving the interplay between tectonics and sedimentation in extensional back-arc basins overlying rheological weak zones inherited from an earlier orogenic evolution are less understood. A typical example is the Pannonian back-arc basin of Central Europe. It is floored by continental lithosphere and was affected by large amounts of extension driven by the subduction rollback that took place in the Carpathians and/or Dinarides. A novel kinematic and seismic sequence stratigraphic interpretation calibrated by wells allows the quantification of the link between the formation of half grabens and coeval sedimentation in the Great Hungarian Plain part of the basin. While the lower order tectonic-induced cycles characterize the main phases of extension in various subbasins, the higher-order cyclicity and associated unconformities define individual moments of fault (re)activation. Our novel interpretation of a temporal and spatial migration of extension during Miocene times explains the contrasting present-day strike of various subbasins as a result of their gradual clockwise rotation. Incorporating the observed asymmetry, in particular the associated footwall exhumation, infers that the amount of extension is much larger than previously thought. The quantitative link between tectonics and sedimentation has allowed the definition of a novel model of sedimentation in asymmetric basins that can be ported to other natural scenarios of similarly hyperextended back-arc basins observed elsewhere. ©2016. American Geophysical Union. All Rights Reserved.},
	keywords = {STRATIGRAPHY; Pannonian Basin; carpathians; Tectonics; Structural geology; Lithology; Sedimentation; Inversion tectonics; Tectonic system; Back-arc extensions; tectonic system tracts; back-arc extension},
	year = {2016},
	eissn = {1944-9194},
	pages = {1526-1559},
	orcid-numbers = {Balázs, Attila/0000-0003-2948-0397}
}

@article{MTMT:3090075,
	title = {Paleogene palaeogeography and basin evolution of the Western Carpathians, Northern Pannonian domain and adjoining areas},
	url = {https://m2.mtmt.hu/api/publication/3090075},
	author = {Kovac, M and Plasienka, D and Soták, J and Vojtko, R and Oszczypko, N and Less, György and Cosovic, V and Fugenschuh, B and Kralikova, S},
	doi = {10.1016/j.gloplacha.2016.03.007},
	journal-iso = {GLOBAL PLANET CHANGE},
	journal = {GLOBAL AND PLANETARY CHANGE},
	volume = {140},
	unique-id = {3090075},
	issn = {0921-8181},
	year = {2016},
	eissn = {1872-6364},
	pages = {9-27}
}

@article{MTMT:3151433,
	title = {Petrology and paleokarst features of the Gomba hydrocarbon reservoir (central Hungary)},
	url = {https://m2.mtmt.hu/api/publication/3151433},
	author = {Bauer, Márton and M. Tóth, Tivadar and Raucsik, Béla and Garaguly, István},
	doi = {10.1556/24.59.2016.003},
	journal-iso = {CENT EUR GEOL},
	journal = {CENTRAL EUROPEAN GEOLOGY},
	volume = {59},
	unique-id = {3151433},
	issn = {1788-2281},
	year = {2016},
	eissn = {1789-3348},
	pages = {28-59},
	orcid-numbers = {M. Tóth, Tivadar/0000-0003-1012-1095; Raucsik, Béla/0000-0002-1951-5974; Garaguly, István/0000-0002-2802-0738}
}

@article{MTMT:3037760,
	title = {Rhinocerotidae from the Upper Miocene deposits of the Western Pannonian Basin},
	url = {https://m2.mtmt.hu/api/publication/3037760},
	author = {Pandolfi, L and Gasparik, Mihály and Magyar, Imre},
	doi = {10.1515/geoca-2016-0004},
	journal-iso = {GEOL CARPATH},
	journal = {GEOLOGICA CARPATHICA},
	volume = {67},
	unique-id = {3037760},
	issn = {1335-0552},
	year = {2016},
	eissn = {1336-8052},
	pages = {69-82}
}

@article{MTMT:2962975,
	title = {Új rétegtani adatok a Zsámbéki-medence triász aljzatából – szerkezetföldtani következtetések},
	url = {https://m2.mtmt.hu/api/publication/2962975},
	author = {Budai, Tamás and Haas, János and Piros, Olga},
	journal-iso = {FÖLDTANI KÖZLÖNY},
	journal = {FÖLDTANI KÖZLÖNY},
	volume = {145},
	unique-id = {2962975},
	issn = {0015-542X},
	year = {2015},
	eissn = {2559-902X},
	pages = {247-257},
	orcid-numbers = {Haas, János/0000-0003-0929-8889}
}

@article{MTMT:2719067,
	title = {Evolution of the Pannonian basin and its geothermal resources},
	url = {https://m2.mtmt.hu/api/publication/2719067},
	author = {Horváth, Ferenc and Musitz, Balázs and Balázs, Attila and Végh, Andor and Uhrin, András and Nádor, Annamária and Koroknai, B and Pap, Norbert and Tóth, Tamás and Wórum, G},
	doi = {10.1016/j.geothermics.2014.07.009},
	journal-iso = {GEOTHERMICS},
	journal = {GEOTHERMICS},
	volume = {53},
	unique-id = {2719067},
	issn = {0375-6505},
	keywords = {Pannonian Basin; Tectonics; Geothermal installations; Thermal water reservoirs},
	year = {2015},
	eissn = {1879-3576},
	pages = {328-352},
	orcid-numbers = {Balázs, Attila/0000-0003-2948-0397; Pap, Norbert/0000-0001-8243-4213}
}

@article{MTMT:2949396,
	title = {Potential maps for the hydrogeologic prerequisites of the installation of deep geothermal doublets and groundwater source heat pump systems in Budapest, Hungary},
	url = {https://m2.mtmt.hu/api/publication/2949396},
	author = {Mádlné Szőnyi, Judit and Virág, Magdolna and Zsemle, Ferenc},
	doi = {10.1556/24.58.2015.1-2.8},
	journal-iso = {CENT EUR GEOL},
	journal = {CENTRAL EUROPEAN GEOLOGY},
	volume = {58},
	unique-id = {2949396},
	issn = {1788-2281},
	year = {2015},
	eissn = {1789-3348},
	pages = {114-128},
	orcid-numbers = {Mádlné Szőnyi, Judit/0000-0002-5628-4386; Virág, Magdolna/0000-0001-6104-1963; Zsemle, Ferenc/0000-0002-1662-4200}
}

@article{MTMT:3089130,
	title = {Sideritic-kaolinitic and green clay layers in the Mecsek Mountains (SW Hungary): Indicators of Middle Triassic volcanism-myth or reality?},
	url = {https://m2.mtmt.hu/api/publication/3089130},
	author = {Lukoczki, Georgina and Budai, Tamás and Németh, Tibor},
	doi = {10.1556/24.58.2015.4.4},
	journal-iso = {CENT EUR GEOL},
	journal = {CENTRAL EUROPEAN GEOLOGY},
	volume = {58},
	unique-id = {3089130},
	issn = {1788-2281},
	year = {2015},
	eissn = {1789-3348},
	pages = {334-355},
	orcid-numbers = {Lukoczki, Georgina/0000-0002-0661-0198; Németh, Tibor/0000-0002-1836-6006}
}

@article{MTMT:2913015,
	title = {Regional underpressure: a factor of uncertainty in the geothermal exploration of deep carbonates, Gödöllő Region, Hungary},
	url = {https://m2.mtmt.hu/api/publication/2913015},
	author = {Mádlné Szőnyi, Judit and Pulay, Eszter and Tóth, Ádám and Kovácsné Bodor, Petra},
	doi = {10.1007/s12665-015-4608-z},
	journal-iso = {ENVIRON EARTH SCI},
	journal = {ENVIRONMENTAL EARTH SCIENCES},
	volume = {74},
	unique-id = {2913015},
	issn = {1866-6280},
	year = {2015},
	eissn = {1866-6299},
	pages = {7523-7538},
	orcid-numbers = {Mádlné Szőnyi, Judit/0000-0002-5628-4386; Tóth, Ádám/0000-0002-7300-6687}
}

@article{MTMT:2934948,
	title = {Turbidites as indicators of paleotopography, Upper Miocene Lake Pannon, Western Mecsek Mountains (Hungary)},
	url = {https://m2.mtmt.hu/api/publication/2934948},
	author = {Sztanó, Orsolya and Sebe, Krisztina and Csillag, Gábor and Magyar, Imre},
	doi = {10.1515/geoca-2015-0029},
	journal-iso = {GEOL CARPATH},
	journal = {GEOLOGICA CARPATHICA},
	volume = {66},
	unique-id = {2934948},
	issn = {1335-0552},
	year = {2015},
	eissn = {1336-8052},
	pages = {331-344},
	orcid-numbers = {Sztanó, Orsolya/0000-0003-0786-3653; Sebe, Krisztina/0000-0002-4647-2199}
}

@article{MTMT:2964506,
	title = {Strike-slip tectonics in the Pannonian basin based on seismic surveys at Lake Balaton},
	url = {https://m2.mtmt.hu/api/publication/2964506},
	author = {Visnovitz, Ferenc and Horváth, Ferenc and Fekete, N and Spiess, V},
	doi = {10.1007/s00531-015-1179-x},
	journal-iso = {INT J EARTH SCI},
	journal = {INTERNATIONAL JOURNAL OF EARTH SCIENCES},
	volume = {104},
	unique-id = {2964506},
	issn = {1437-3254},
	abstract = {Strike-slip tectonics has been the dominant style of deformation during the neotectonic (Pliocene and Quaternary) evolution of the Pannonian basin. Main faults are exposed in the “island mountains” of the basin, but strike-slip tectonic features can be best studied in the basin fill by seismic data. Lake Balaton offers the opportunity to carry out high to ultra-high-resolution seismo-acoustic surveys to image stratigraphic and tectonic features in the central part of the Pannonian basin. Several campaigns in the lake using different acquisition techniques have resulted in more than 2000-km seismo-acoustic profiles with a range of resolutions and penetration depths. Interpretation of faults and folds shows a few kilometers wide shear zone below the lake in Late Miocene–Pliocene strata. This zone can be identified as the continuation of the Balatonfő line known onshore to the east of the lake. Mapping revealed a set of duplex structures and highlighted the importance of this shear zone in the formation of Lake Balaton. Comparison of our results to analogue clay models suggests that the observed shear zone is sinistral and the horizontal displacement is on the order of hundreds of meters. Looking at 3D industrial seismic data to the south of the lake, we suggest that the first-order Balaton line, which represents the continuation of Periadriatic line, is also sinistral and characterized by small horizontal displacement of about 1.0–1.5 km during Pliocene and Quaternary times. This indicates a 0.2–0.3 mm/year average slip rate, which is compatible with recent GPS measurements.},
	year = {2015},
	eissn = {1437-3262},
	pages = {2273-2285},
	orcid-numbers = {Visnovitz, Ferenc/0000-0002-7040-0080}
}

@article{MTMT:2711228,
	title = {Red calcite: an indicator of paleo-karst systems associated with bauxitic unconformities},
	url = {https://m2.mtmt.hu/api/publication/2711228},
	author = {Győri, Orsolya and Orbán, Richárd and Mindszenty, Andrea and Fodor, László and Poros, Zsófia and Erőss, Anita and Benkó, Zsolt and Molnár, Ferenc},
	doi = {10.1111/gfl.12088},
	journal-iso = {GEOFLUIDS},
	journal = {GEOFLUIDS},
	volume = {14},
	unique-id = {2711228},
	issn = {1468-8115},
	year = {2014},
	eissn = {1468-8123},
	pages = {459-480},
	orcid-numbers = {Győri, Orsolya/0000-0002-3646-9113; Mindszenty, Andrea/0000-0001-8927-3053; Erőss, Anita/0000-0002-2395-3934; Molnár, Ferenc/0000-0002-1873-1915}
}

@article{MTMT:2953617,
	title = {Re-evaluation of the Triassic sequence in the subsurface of the Little Plain Basin Hungary. A case study from the Győrszemere-2 well},
	url = {https://m2.mtmt.hu/api/publication/2953617},
	author = {Velledits, Felicitász and Csizmeg, János and Oravecz-Scheffer, Anna},
	doi = {10.1556/CEuGeol.57.2014.4.2},
	journal-iso = {CENT EUR GEOL},
	journal = {CENTRAL EUROPEAN GEOLOGY},
	volume = {57},
	unique-id = {2953617},
	issn = {1788-2281},
	year = {2014},
	eissn = {1789-3348},
	pages = {345-362}
}

@book{MTMT:2584586,
	title = {Budapest: földtani értékek és az ember. Városgeológiai tanulmányok („In urbe et pro urbe”)},
	url = {https://m2.mtmt.hu/api/publication/2584586},
	isbn = {9789632843681},
	editor = {Mindszenty, Andrea},
	publisher = {ELTE Eötvös Kiadó Kft.},
	unique-id = {2584586},
	year = {2013},
	orcid-numbers = {Mindszenty, Andrea/0000-0001-8927-3053}
}

@article{MTMT:2414426,
	title = {The origin and role of a calcite-filled microcrack generation in a metamorphic crystalline complex: The characterization of a fossilised seismic permeability system},
	url = {https://m2.mtmt.hu/api/publication/2414426},
	author = {Dabi, Gergely and Bajnóczi, Bernadett and Schubert, Félix and M. Tóth, Tivadar},
	doi = {10.1016/j.tecto.2013.07.039},
	journal-iso = {TECTONOPHYSICS},
	journal = {TECTONOPHYSICS},
	volume = {608},
	unique-id = {2414426},
	issn = {0040-1951},
	year = {2013},
	eissn = {1879-3266},
	pages = {792-803},
	orcid-numbers = {Bajnóczi, Bernadett/0000-0003-0006-7611; Schubert, Félix/0000-0001-8647-5354; M. Tóth, Tivadar/0000-0003-1012-1095}
}

@article{MTMT:2420373,
	title = {A Mura-Zala-medence vízföldtani elemzést szolgáló földtani-szerkezetföldtani modellje},
	url = {https://m2.mtmt.hu/api/publication/2420373},
	author = {Fodor, László and Uhrin, András and Palotás, Klára and Selmeczi, Ildikó and Tóthné, M Á and Riznar, I and Trajanova, M and Rifelj, H and Jelen, B and Budai, Tamás and Koroknai, B and Mozetic, S and Nádor, Annamária and Lapanje, A},
	journal-iso = {M ÁLL FÖLDT INT JELENT},
	journal = {MAGYAR ÁLLAMI FÖLDTANI INTÉZET ÉVI JELENTÉSE},
	volume = {2011},
	unique-id = {2420373},
	issn = {0368-9751},
	year = {2013},
	pages = {47-91}
}

@article{MTMT:2174035,
	title = {Transboundary geothermal resources of the Mura-Zala basin: a need for joint thermal aquifer management of Slovenia and Hungary = Čezmejni geotermalni viri Mursko-Zalskega bazena: potreba po skupnem upravljanju geotermalnih vodonosnikov Slovenije in Madžarske},
	url = {https://m2.mtmt.hu/api/publication/2174035},
	author = {Nádor, Annamária and Lapanje, A and Tóth, György and Rman, N and Szőcs, Teodóra and Prestor, J and Uhrin, András and Rajver, D and Fodor, László and Muráti, J and Székely, E},
	doi = {10.5474/geologija.2012.013},
	journal-iso = {GEOLOGIJA (LJUBLJANA)},
	journal = {GEOLOGIJA (LJUBLJANA)},
	volume = {55},
	unique-id = {2174035},
	issn = {0016-7789},
	year = {2012},
	eissn = {1854-620X},
	pages = {209-223}
}

@article{MTMT:2384730,
	title = {Flexural basin reworked by salt-related pull-apart structures: the Adony Basin.},
	url = {https://m2.mtmt.hu/api/publication/2384730},
	author = {Palotai, Márton and Csontos, L},
	doi = {10.1556/CEuGeol.55.2012.2.3},
	journal-iso = {CENT EUR GEOL},
	journal = {CENTRAL EUROPEAN GEOLOGY},
	volume = {55},
	unique-id = {2384730},
	issn = {1788-2281},
	year = {2012},
	eissn = {1789-3348},
	pages = {147-180}
}

@article{MTMT:1791294,
	title = {Displaced South Alpine and Dinaridic elements in the Mid-Hungarian Zone},
	url = {https://m2.mtmt.hu/api/publication/1791294},
	author = {Kovács, S and Haas, János},
	doi = {10.1556/CEuGeol.53.2010.2-3.3},
	journal-iso = {CENT EUR GEOL},
	journal = {CENTRAL EUROPEAN GEOLOGY},
	volume = {53},
	unique-id = {1791294},
	issn = {1788-2281},
	year = {2010},
	eissn = {1789-3348},
	pages = {135-164},
	orcid-numbers = {Haas, János/0000-0003-0929-8889}
}