@article{MTMT:30899104,
	title = {Dolomitization of shallow-water, mixed silicilastic‑carbonate sequences: The Lower Triassic ramp succession of the Transdanubian Range, Hungary},
	url = {https://m2.mtmt.hu/api/publication/30899104},
	author = {Győri, Orsolya and Haas, János and Hips, Kinga and Lukoczki, Georgina and Budai, Tamás and Demény, Attila and Laczkó-Dobos, Emese},
	doi = {10.1016/j.sedgeo.2019.105549},
	journal-iso = {SEDIMENT GEOL},
	journal = {SEDIMENTARY GEOLOGY},
	volume = {395},
	unique-id = {30899104},
	issn = {0037-0738},
	abstract = {The Lower Triassic succession of the Transdanubian Range in Hungary comprises limestones, dolomite, marl, sandstones and siltstones, deposited in tidal flat, lagoon and ooid shoal environments on the marginal ramp of the western Neotethys. Seven cores were chosen for petrographic and stable isotope investigations aiming to reconstruct the paragenetic sequence with special regard to the dolomitization and hydrothermal events. Five lithotypes were differentiated: (i) dolomite, (ii) sandy, silty, clayey dolomite, and dolomarl, (iii), dolomitic siltstone and sandstone, (iv) dolomitic limestone, and (v) limestone. In these lithotypes, three types of dolomites are present: non-ferroan replacive, ferroan replacive, and ferroan cement. Fabric retentive and fabric destructive non-ferroan replacive dolomitization are interpreted to have occurred by seepage reflux. Supporting evidence includes the presence gypsum and anhydrite in the Lower Triassic beds. Stable isotope values of the ferroan dolomite (delta O-18 of -10.7 to -4.2 parts per thousand and delta C-13 of 4.8 to 4.7 parts per thousand) suggest dolomitization by fluids of relatively high temperature. The similar stable isotope values (delta O-18 of -9.3 to -5.8 parts per thousand and delta C-13 of -1.9 to 2.5 parts per thousand) of the non-ferroan dolomite phase suggest that the reflux dolomite was overprinted by this second dolomitization event. Traces of exotic minerals, such as barite, chalcopyrite, galena and sulphosalts were found as fillings of vugs and fractures in the dolomite-cemented sandstone. The metals could have been sourced from the underlying Permian red sandstone beds. The heterogeneous sediment composition had profound impact on the diagenesis of these sedimentary successions.},
	year = {2020},
	eissn = {1879-0968},
	orcid-numbers = {Győri, Orsolya/0000-0002-3646-9113; Haas, János/0000-0003-0929-8889; Hips, Kinga/0000-0003-2315-120X; Lukoczki, Georgina/0000-0002-0661-0198; Demény, Attila/0000-0003-0522-9018}
}

@article{MTMT:31620127,
	title = {Karbonátos konkréciók az alsó-miocén Pétervásárai Homokkő Formációban (Pétervásárai-dombság, Leleszi-völgy). genetikai megfontolások morfológiai és petrográfiai vizsgálatok eredményei alapján},
	url = {https://m2.mtmt.hu/api/publication/31620127},
	author = {Veres, Zsolt and Raucsikné Varga, Andrea Beáta},
	doi = {10.23928/foldt.kozl.2020.150.3.429},
	journal-iso = {FÖLDTANI KÖZLÖNY},
	journal = {FÖLDTANI KÖZLÖNY},
	volume = {150},
	unique-id = {31620127},
	issn = {0015-542X},
	year = {2020},
	eissn = {2559-902X},
	pages = {429-447},
	orcid-numbers = {Raucsikné Varga, Andrea Beáta/0000-0002-8673-1482}
}

@article{MTMT:30635811,
	title = {Deformation band formation as a function of progressive burial: Depth calibration and mechanism change in the Pannonian Basin (Hungary)},
	url = {https://m2.mtmt.hu/api/publication/30635811},
	author = {Beke, Barbara and Fodor, László and Millar, L and Petrik, Attila},
	doi = {10.1016/j.marpetgeo.2019.04.006},
	journal-iso = {MAR PETROL GEOL},
	journal = {MARINE AND PETROLEUM GEOLOGY},
	volume = {105},
	unique-id = {30635811},
	issn = {0264-8172},
	abstract = {Deformation bands (DB) are ubiquitous structural elements that can be found in Miocene pre- and syn-rift sediments of the extensional Pannonian Basin, central Europe. Across the field sites we see examples of disaggregation to cataclastic DB sets and evidence of frequent reactivation by discrete faulting. Thin section analysis, cross-cutting relationships and well-defined time constraints of analysed brittle structures demonstrate that with increased burial depth, DB deformation mechanisms progressed from granular flow to cataclasis.
		
		The DB sets were classified into 10 deformation phases based on formerly published independent fault-slip analysis and structural mapping. Subsidence curves were constructed for each stratigraphic level involved in deformation and were used along with the intersection of deformation episodes to calculate the depth intervals of DB generations and subsequent structural elements. The DB formation depths obtained were transferred to the depth range of the related mechanisms. This combined methodology permits a more quantitative approach to determine the changes in the deformation mechanisms with depth.
		
		Our results show that granular flow (disaggregation bands) dominates down to 100-150 m as the earliest deformation structure, followed by weak then moderate cataclasis. The transition between weak and moderate cataclasis is at approximately 300 +/- 100 m for host rock rich in feldspar or fragile tuffitic components and from around 900 +/- 100 m in quartz-rich sediments. In addition, deformation by frictional sliding concentrates on discrete fault planes at the margin of cataclastic bands or on new fracture planes from similar to 500 +/- 100 m in volcanoclastic or feldspar rich host rocks, and 1000 +/- 100 m in quartz-rich host rocks.
		
		We suggest that burial-induced diagenetic processes is dependent on subsidence history, and partly in connection with regional fluid migration path, control the transition from moderate or advanced cataclasis to discrete fault slip. All these changes affect the pore structure and porosity that contribute to rheological changes, and hence change in deformation mechanism of coeval fracturing events.},
	year = {2019},
	eissn = {1873-4073},
	pages = {1-16},
	orcid-numbers = {Beke, Barbara/0000-0003-0797-1195; Petrik, Attila/0000-0001-6164-1758}
}

@article{MTMT:31029800,
	title = {Granulometric properties of particles in Upper Miocene sandstones from thin sections, Szolnok Formation, Hungary},
	url = {https://m2.mtmt.hu/api/publication/31029800},
	author = {Király, Csilla and Falus, György and Gresina, Fruzsina and Jakab, Gergely Imre and Szalai, Zoltán and Varga, György},
	doi = {10.15201/hungeobull.68.4.2},
	journal-iso = {HUNG GEOGR BULL (2009-)},
	journal = {HUNGARIAN GEOGRAPHICAL BULLETIN (2009-)},
	volume = {68},
	unique-id = {31029800},
	issn = {2064-5031},
	keywords = {sandstones; Upper Miocene},
	year = {2019},
	eissn = {2064-5147},
	pages = {341-353},
	orcid-numbers = {Jakab, Gergely Imre/0000-0001-5424-1983; Szalai, Zoltán/0000-0001-5267-411X; Varga, György/0000-0003-4784-6372}
}

@CONFERENCE{MTMT:30753158,
	title = {Diagenetic evolution of the sandstone member of Kosd Formation (Central Hungary)},
	url = {https://m2.mtmt.hu/api/publication/30753158},
	author = {Körmös, Sándor and Raucsikné Varga, Andrea Beáta and Radovics, Balázs Géza and Schubert, Félix},
	booktitle = {EGU (European Geosciences Union) General Assembly 2019},
	unique-id = {30753158},
	year = {2019},
	orcid-numbers = {Körmös, Sándor/0000-0003-4439-6804; Raucsikné Varga, Andrea Beáta/0000-0002-8673-1482; Schubert, Félix/0000-0001-8647-5354}
}

@article{MTMT:30644307,
	title = {Cements, Waters, and Scales: An Integrated Study of the Szeged Geothermal Systems (SE Hungary) to Characterize Natural Environmental Conditions of the Thermal Aquifer},
	url = {https://m2.mtmt.hu/api/publication/30644307},
	author = {Raucsikné Varga, Andrea Beáta and Bozsó, Gábor and Garaguly, István and Raucsik, Béla and Bencsik, Attila and Kóbor, Balázs},
	doi = {10.1155/2019/4863814},
	journal-iso = {GEOFLUIDS},
	journal = {GEOFLUIDS},
	volume = {2019},
	unique-id = {30644307},
	issn = {1468-8115},
	year = {2019},
	eissn = {1468-8123},
	orcid-numbers = {Raucsikné Varga, Andrea Beáta/0000-0002-8673-1482; Garaguly, István/0000-0002-2802-0738; Raucsik, Béla/0000-0002-1951-5974}
}

@article{MTMT:30417004,
	title = {Multiphase carbonate cementation in the Miocene Pétervására Sandstone (North Hungary): implications for basinal fluid flow and burial history},
	url = {https://m2.mtmt.hu/api/publication/30417004},
	author = {Laczkó-Dobos, Emese and Hips, Kinga},
	doi = {10.1515/geoca-2018-0030},
	journal-iso = {GEOL CARPATH},
	journal = {GEOLOGICA CARPATHICA},
	volume = {69},
	unique-id = {30417004},
	issn = {1335-0552},
	year = {2018},
	eissn = {1336-8052},
	pages = {515-527},
	orcid-numbers = {Hips, Kinga/0000-0003-2315-120X}
}

@article{MTMT:3273982,
	title = {Tracing multiple resedimentation on an isolated karstified plateau: The bauxite-bearing Miocene red clay of the Southern Bakony Mountains, Hungary},
	url = {https://m2.mtmt.hu/api/publication/3273982},
	author = {Kelemen, Péter and Dunkl, István and Csillag, Gábor and Mindszenty, Andrea and von Eynatten, H and Józsa, Sándor},
	doi = {10.1016/j.sedgeo.2017.07.005},
	journal-iso = {SEDIMENT GEOL},
	journal = {SEDIMENTARY GEOLOGY},
	volume = {358},
	unique-id = {3273982},
	issn = {0037-0738},
	keywords = {SYSTEM; DISTRIBUTIONS; PROVENANCE; WESTERN HUNGARY; Pannonian Basin; Neogene; magmatism; ALPS; ZIRCON; Transdanubian range; Bakony Mountains; BAUXITE; ROCKS; U-Pb geochronology; U-PB; Continental sedimentation},
	year = {2017},
	eissn = {1879-0968},
	pages = {84-96},
	orcid-numbers = {Mindszenty, Andrea/0000-0001-8927-3053; Józsa, Sándor/0000-0001-8219-0044}
}

@mastersthesis{MTMT:3321895,
	title = {Mihályi-Répcelak természetes CO2-előfordulás környezetgeokémiai vizsgálata},
	url = {https://m2.mtmt.hu/api/publication/3321895},
	author = {Király, Csilla},
	doi = {10.15476/ELTE.2017.032},
	publisher = {Eötvös Loránd University},
	unique-id = {3321895},
	keywords = {széndioxid; Doktori disszertáció; Mihályi-Répcelak; környezetgeokémia},
	year = {2017}
}

@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:3309676,
	title = {Jégszállította dumortierites gneisz, klinohumitos márvány és szkapolitos amfibolit a Duna pleisztocén kavicsanyagában},
	url = {https://m2.mtmt.hu/api/publication/3309676},
	author = {Spránitz, Tamás and Váczi, Benjámin and Lange, Thomas Pieter and Józsa, Sándor},
	doi = {10.23928/foldt.kozl.2017.147.3.311},
	journal-iso = {FÖLDTANI KÖZLÖNY},
	journal = {FÖLDTANI KÖZLÖNY},
	volume = {147},
	unique-id = {3309676},
	issn = {0015-542X},
	year = {2017},
	eissn = {2559-902X},
	pages = {311-326},
	orcid-numbers = {Spránitz, Tamás/0000-0002-5086-3133; Lange, Thomas Pieter/0000-0002-8709-9239; Józsa, Sándor/0000-0001-8219-0044}
}

@article{MTMT:3143517,
	title = {Pleisztocén folyóvízi kavics a Villányi-hegységben},
	url = {https://m2.mtmt.hu/api/publication/3143517},
	author = {Szujó, Gábor Lajos and Sebe, Krisztina and Sipos, György and Pozsgai, Emília},
	doi = {10.23928/foldt.kozl.2017.147.1.85},
	journal-iso = {FÖLDTANI KÖZLÖNY},
	journal = {FÖLDTANI KÖZLÖNY},
	volume = {147},
	unique-id = {3143517},
	issn = {0015-542X},
	year = {2017},
	eissn = {2559-902X},
	pages = {85-98},
	orcid-numbers = {Sebe, Krisztina/0000-0002-4647-2199; Sipos, György/0000-0001-6224-2361}
}

@article{MTMT:3202159,
	title = {Az Endrődi Formáció kőzettani és palinológiai vizsgálata a Hódmezővásárhely–I fúrásban (Makói-árok) — őskörnyezeti és diagenezis-történeti értékelés},
	url = {https://m2.mtmt.hu/api/publication/3202159},
	author = {Raucsikné Varga, Andrea Beáta and Baranyi, Viktória and Raucsik, Béla and Schubert, Félix},
	doi = {10.23928/foldt.kozl.2017.147.1.61},
	journal-iso = {FÖLDTANI KÖZLÖNY},
	journal = {FÖLDTANI KÖZLÖNY},
	volume = {147},
	unique-id = {3202159},
	issn = {0015-542X},
	year = {2017},
	eissn = {2559-902X},
	pages = {61-84},
	orcid-numbers = {Raucsikné Varga, Andrea Beáta/0000-0002-8673-1482; Baranyi, Viktória/0000-0002-1194-9903; Raucsik, Béla/0000-0002-1951-5974; Schubert, Félix/0000-0001-8647-5354}
}

@article{MTMT:3219126,
	title = {A Reiflingi esemény hatása az Északi-Mészkőalpok és az Aggteleki-hegység középső-triász fejlődésére},
	url = {https://m2.mtmt.hu/api/publication/3219126},
	author = {Velledits, Felicitász and Richard, Lein and Leopold, Krystyn and Péró, Csaba and Piros, Olga and Joachim, Blau},
	doi = {10.23928/foldt.kozl.2017.147.1.3},
	journal-iso = {FÖLDTANI KÖZLÖNY},
	journal = {FÖLDTANI KÖZLÖNY},
	volume = {147},
	unique-id = {3219126},
	issn = {0015-542X},
	year = {2017},
	eissn = {2559-902X},
	pages = {3-24}
}

@article{MTMT:3193579,
	title = {Rezervoár analóg pannóniai turbiditek Kelet-Erdélyben: őskörnyezet és porozitásfejlődés},
	url = {https://m2.mtmt.hu/api/publication/3193579},
	author = {Bartha, István Róbert and Laczkó-Dobos, Emese and Tőkés, Lilla},
	journal-iso = {FÖLDTANI KÖZLÖNY},
	journal = {FÖLDTANI KÖZLÖNY},
	volume = {146},
	unique-id = {3193579},
	issn = {0015-542X},
	year = {2016},
	eissn = {2559-902X},
	pages = {257-274},
	orcid-numbers = {Bartha, István Róbert/0000-0003-3198-2687; Tőkés, Lilla/0000-0002-2518-9431}
}

@article{MTMT:3167421,
	title = {Re-evaluation of archive pebble distribution data for the Upper Permian Bakonya Sandstone Member of the Kővágószőlős Formation, Hungary — a comparison with the composition of cores BAF–1 and BAF–1A},
	url = {https://m2.mtmt.hu/api/publication/3167421},
	author = {Magyar, Levente and Benei, Balázs and Halász, Amadé},
	journal-iso = {FÖLDTANI KÖZLÖNY},
	journal = {FÖLDTANI KÖZLÖNY},
	volume = {146},
	unique-id = {3167421},
	issn = {0015-542X},
	year = {2016},
	eissn = {2559-902X},
	pages = {223-232},
	orcid-numbers = {Halász, Amadé/0000-0003-4582-8883}
}

@article{MTMT:27184471,
	title = {A Budai-hegység felső-eocén összletének bázisán települő lávakőzet- és tufaklasztokat tartalmazó törmelékes üledékes kőzetek petrográfiai jellegei},
	url = {https://m2.mtmt.hu/api/publication/27184471},
	author = {Farics, Éva and Józsa, Sándor and Haas, János},
	journal-iso = {FÖLDTANI KÖZLÖNY},
	journal = {FÖLDTANI KÖZLÖNY},
	volume = {145},
	unique-id = {27184471},
	issn = {0015-542X},
	year = {2015},
	eissn = {2559-902X},
	pages = {331-350},
	orcid-numbers = {Józsa, Sándor/0000-0001-8219-0044; Haas, János/0000-0003-0929-8889}
}

@article{MTMT:2994553,
	title = {A Visegrádi-szoros kiemelt helyzetű kavicsos üledékeinek vizsgálata Zebegény térségében, és jelentősége a magas dunai teraszok morfosztratigráfiai besorolásakor},
	url = {https://m2.mtmt.hu/api/publication/2994553},
	author = {Szeberényi, József and Józsa, Sándor and Simon, I and Kiss, Klaudia and Bradák, Balázs and Viczián, István},
	journal-iso = {FÖLDTANI KÖZLÖNY},
	journal = {FÖLDTANI KÖZLÖNY},
	volume = {145},
	unique-id = {2994553},
	issn = {0015-542X},
	year = {2015},
	eissn = {2559-902X},
	pages = {367-383},
	orcid-numbers = {Józsa, Sándor/0000-0001-8219-0044}
}

@article{MTMT:2996607,
	title = {A kora-miocén Pétervásárai Homokkő diagenezis-története [Diagenetic evolution of the lower miocene pétervására sandstone formation]},
	url = {https://m2.mtmt.hu/api/publication/2996607},
	author = {Laczkó-Dobos, Emese and Hips, Kinga and Józsa, Sándor and Bendő, Zsolt},
	journal-iso = {FÖLDTANI KÖZLÖNY},
	journal = {FÖLDTANI KÖZLÖNY},
	volume = {145},
	unique-id = {2996607},
	issn = {0015-542X},
	year = {2015},
	eissn = {2559-902X},
	pages = {351-366},
	orcid-numbers = {Hips, Kinga/0000-0003-2315-120X; Józsa, Sándor/0000-0001-8219-0044}
}

@inproceedings{MTMT:2852139,
	title = {A dél-alföldi permo-mezozoos képződmények: a diagenezis-történet jellemzése és előzetes regionális korreláció kőzettani és geokémiai eredmények alapján},
	url = {https://m2.mtmt.hu/api/publication/2852139},
	author = {Raucsikné Varga, Andrea Beáta and Pál-Molnár, Elemér and Raucsik, Béla and Schubert, Félix and Garaguly, István and Haranginé Lukács, Réka and Kiss, Balázs},
	booktitle = {Tisia Konferencia},
	unique-id = {2852139},
	year = {2015},
	pages = {17-20},
	orcid-numbers = {Raucsikné Varga, Andrea Beáta/0000-0002-8673-1482; Pál-Molnár, Elemér/0000-0002-9606-0133; Raucsik, Béla/0000-0002-1951-5974; Schubert, Félix/0000-0001-8647-5354; Garaguly, István/0000-0002-2802-0738; Haranginé Lukács, Réka/0000-0002-2338-4209; Kiss, Balázs/0000-0003-0040-0656}
}

@misc{MTMT:3416391,
	title = {A Szegedi-medence és közvetlen környezetének diagenezis-történet és mikrotektonikai vizsgálata. Ásotthalom-Mórahalom mintaterület},
	url = {https://m2.mtmt.hu/api/publication/3416391},
	author = {Raucsikné Varga, Andrea Beáta and Raucsik, Béla and Schubert, Félix and Garaguly, I and Mészáros, E and Fiser-Nagy, Á and Dabi, G},
	unique-id = {3416391},
	year = {2015},
	orcid-numbers = {Raucsikné Varga, Andrea Beáta/0000-0002-8673-1482; Raucsik, Béla/0000-0002-1951-5974; Schubert, Félix/0000-0001-8647-5354}
}

@article{MTMT:2462162,
	title = {A budai Mátyás-hegy bryozoás márga összletébe települt vulkanogén képződmény kőzettani-vulkanológiai vizsgálata},
	url = {https://m2.mtmt.hu/api/publication/2462162},
	author = {Biró, Tamás and Józsa, Sándor and Karátson, Dávid and Szenthe, I},
	journal-iso = {FÖLDTANI KÖZLÖNY},
	journal = {FÖLDTANI KÖZLÖNY},
	volume = {143},
	unique-id = {2462162},
	issn = {0015-542X},
	year = {2014},
	eissn = {2559-902X},
	pages = {239-250},
	orcid-numbers = {Biró, Tamás/0000-0001-5198-7210; Józsa, Sándor/0000-0001-8219-0044; Karátson, Dávid/0000-0003-0386-1239}
}

@article{MTMT:2497605,
	title = {Different paleoenvironments of Late Pleistocene age identified in Verőce outcrop, Hungary. preliminary results},
	url = {https://m2.mtmt.hu/api/publication/2497605},
	author = {Bradák, Balázs and Kiss, Klaudia and Barta, Gabriella and Varga, György and Szeberényi, József and Józsa, Sándor and Novothny, Ágnes and Kovács, József and Markó, András and Mészáros, Erzsébet and Szalai, Zoltán},
	doi = {10.1016/j.quaint.2013.11.035},
	journal-iso = {QUATERN INT},
	journal = {QUATERNARY INTERNATIONAL},
	volume = {319},
	unique-id = {2497605},
	issn = {1040-6182},
	year = {2014},
	eissn = {1873-4553},
	pages = {119-136},
	orcid-numbers = {Barta, Gabriella/0000-0002-5460-1085; Varga, György/0000-0003-4784-6372; Józsa, Sándor/0000-0001-8219-0044; Novothny, Ágnes/0000-0003-3513-0406; Kovács, József/0000-0002-6797-2504; Markó, András/0000-0002-7556-0091; Szalai, Zoltán/0000-0001-5267-411X}
}

@inproceedings{MTMT:2805058,
	title = {Dunateraszok helyzete a Visegrádi-szorosban},
	url = {https://m2.mtmt.hu/api/publication/2805058},
	author = {Szeberényi, József and Józsa, Sándor and Medved’ová, A and Holec, J and Balogh, János and Fábián, Szabolcs Ákos and Kis, Éva and Varga, György and Viczián, István},
	booktitle = {VII. Magyar Földrajzi Konferencia kiadványa},
	unique-id = {2805058},
	year = {2014},
	pages = {513-527},
	orcid-numbers = {Józsa, Sándor/0000-0001-8219-0044; Fábián, Szabolcs Ákos/0000-0001-9127-2113; Varga, György/0000-0003-4784-6372}
}

@article{MTMT:2793454,
	title = {Az alsó-permi Korpádi Homokkő Formáció törmelékes kőzeteinek ásványtani és kőzettani jellemzői a Túrony–1 fúrásban (Szlavóniai–Drávai-terrénum) [Mineralogical and petrographic characteristics of siliciclastic rocks from the lower permian korpád sandstone formation of borehole túrony-1 (slavonia-dráva unit)]},
	url = {https://m2.mtmt.hu/api/publication/2793454},
	author = {Raucsikné Varga, Andrea Beáta and Raucsik, Béla and Szakmány, György},
	journal-iso = {FÖLDTANI KÖZLÖNY},
	journal = {FÖLDTANI KÖZLÖNY},
	volume = {144},
	unique-id = {2793454},
	issn = {0015-542X},
	year = {2014},
	eissn = {2559-902X},
	pages = {211-230},
	orcid-numbers = {Raucsikné Varga, Andrea Beáta/0000-0002-8673-1482; Raucsik, Béla/0000-0002-1951-5974; Szakmány, György/0000-0002-9557-2030}
}

@article{MTMT:30937292,
	title = {Pedogenic calcrete records in southern Transdanubia, Hungary: A brief review with paleoenvironmental and paleogeographic implications},
	url = {https://m2.mtmt.hu/api/publication/30937292},
	author = {Raucsikné Varga, Andrea Beáta and Raucsik, Béla},
	doi = {10.1556/CEuGeol.57.2014.2.2},
	journal-iso = {CENT EUR GEOL},
	journal = {CENTRAL EUROPEAN GEOLOGY},
	volume = {57},
	unique-id = {30937292},
	issn = {1788-2281},
	year = {2014},
	eissn = {1789-3348},
	pages = {137-151},
	orcid-numbers = {Raucsikné Varga, Andrea Beáta/0000-0002-8673-1482; Raucsik, Béla/0000-0002-1951-5974}
}

@article{MTMT:2480410,
	title = {Homokos talajok összehasonlító ásványtani és szemcsemorfológiai vizsgálata tiszántúli erdős és füves területeken},
	url = {https://m2.mtmt.hu/api/publication/2480410},
	author = {Balog, Kitti and Kalmár, János and Kuti, László and Szabó, András and Fodor, Nándor and Tóth, Tibor},
	doi = {10.1556/Agrokem.62.2013.2.7},
	journal-iso = {AGROKÉMIA ÉS TALAJTAN},
	journal = {AGROKÉMIA ÉS TALAJTAN},
	volume = {62},
	unique-id = {2480410},
	issn = {0002-1873},
	year = {2013},
	eissn = {1588-2713},
	pages = {267-284},
	orcid-numbers = {Balog, Kitti/0000-0001-9183-5529}
}

@article{MTMT:2748939,
	title = {Deformációs szalagok porózus kőzetekben},
	url = {https://m2.mtmt.hu/api/publication/2748939},
	author = {Beke, Barbara and Fodor, László},
	journal-iso = {FÖLDTANI KÖZLÖNY},
	journal = {FÖLDTANI KÖZLÖNY},
	volume = {144},
	unique-id = {2748939},
	issn = {0015-542X},
	year = {2013},
	eissn = {2559-902X},
	pages = {255-274},
	orcid-numbers = {Beke, Barbara/0000-0003-0797-1195}
}

@article{MTMT:2957981,
	title = {A regölyi kora vaskori sírhalom kőzetleleteinek előzetes archeometriai vizsgálati eredményei.},
	url = {https://m2.mtmt.hu/api/publication/2957981},
	author = {Kürthy, Dóra and Szakmány, György and Józsa, Sándor and Szabó, G},
	journal-iso = {ARCHEOMETRIAI MŰHELY},
	journal = {ARCHEOMETRIAI MŰHELY},
	volume = {10},
	unique-id = {2957981},
	issn = {1786-271X},
	year = {2013},
	pages = {111-125},
	orcid-numbers = {Kürthy, Dóra/0009-0001-3206-1495; Szakmány, György/0000-0002-9557-2030; Józsa, Sándor/0000-0001-8219-0044}
}

@CONFERENCE{MTMT:2448479,
	title = {Agyagásványtani és petrográfiai vizsgálatok új szemléletű értelmezése a Makói-árok túlnyomásos zónáiból (Endrődi Formáció, Pannon-medence, Magyarország)},
	url = {https://m2.mtmt.hu/api/publication/2448479},
	author = {Tóth, F and Raucsikné Varga, Andrea Beáta and Raucsik, Béla},
	booktitle = {XV. Székelyföldi Geológus Találkozó},
	unique-id = {2448479},
	year = {2013},
	pages = {74-75},
	orcid-numbers = {Raucsikné Varga, Andrea Beáta/0000-0002-8673-1482; Raucsik, Béla/0000-0002-1951-5974}
}

@article{MTMT:2008179,
	title = {"Ízesítő" a permi Bodai Agyagkő Formáció őskörnyezeti rekonstrukciójához: kősó utáni pszeudomorfózák a BAT-4 fúrás agyagkőmintáiban},
	url = {https://m2.mtmt.hu/api/publication/2008179},
	author = {Máthé, Zoltán and Raucsikné Varga, Andrea Beáta},
	journal-iso = {FÖLDTANI KÖZLÖNY},
	journal = {FÖLDTANI KÖZLÖNY},
	volume = {142},
	unique-id = {2008179},
	issn = {0015-542X},
	year = {2012},
	eissn = {2559-902X},
	pages = {201-204},
	orcid-numbers = {Raucsikné Varga, Andrea Beáta/0000-0002-8673-1482}
}

@article{MTMT:3072470,
	title = {Balatonőszöd – Temetői dűlő rézkori lelőhely homokkő nyersanyagú kőeszközeinek kőzettani és geokémiai vizsgálata. / Petrographical and Geochemical investigation of stone tools made of sandstone from the site Balatonőszöd – Temetői dűlő (Hungary)},
	url = {https://m2.mtmt.hu/api/publication/3072470},
	author = {Péterdi, Bálint},
	journal-iso = {ARCHEOMETRIAI MŰHELY},
	journal = {ARCHEOMETRIAI MŰHELY},
	volume = {9},
	unique-id = {3072470},
	issn = {1786-271X},
	year = {2012},
	pages = {265-286}
}

@article{MTMT:1930795,
	title = {Cirkon egykristály U-Pb korok a danitzpusztai pannóniai homokból: közvetett bizonyítékok az aljzatot alkotó metamorfitok kevert prevariszkuszi protolitjaira},
	url = {https://m2.mtmt.hu/api/publication/1930795},
	author = {Raucsikné Varga, Andrea Beáta and Újvári, Gábor and Kovács, János},
	journal-iso = {FÖLDTANI KÖZLÖNY},
	journal = {FÖLDTANI KÖZLÖNY},
	volume = {142},
	unique-id = {1930795},
	issn = {0015-542X},
	year = {2012},
	eissn = {2559-902X},
	pages = {95-98},
	orcid-numbers = {Raucsikné Varga, Andrea Beáta/0000-0002-8673-1482; Újvári, Gábor/0000-0002-2816-6155; Kovács, János/0000-0001-7742-5515}
}

@article{MTMT:2157138,
	title = {Nodular calcrete from the Lower Permian Korpád Sandstone Formation (borehole Dinnyeberki 9015, Mecsek Mts, Hungary) and its palaeoenvironmental significance},
	url = {https://m2.mtmt.hu/api/publication/2157138},
	author = {Raucsikné Varga, Andrea Beáta and Raucsik, Béla and Bajnóczi, Bernadett},
	journal-iso = {FÖLDTANI KÖZLÖNY},
	journal = {FÖLDTANI KÖZLÖNY},
	volume = {142},
	unique-id = {2157138},
	issn = {0015-542X},
	year = {2012},
	eissn = {2559-902X},
	pages = {375-378},
	orcid-numbers = {Raucsikné Varga, Andrea Beáta/0000-0002-8673-1482; Raucsik, Béla/0000-0002-1951-5974; Bajnóczi, Bernadett/0000-0003-0006-7611}
}

@article{MTMT:1339707,
	title = {Multiple provenance of detrital zircons from the Permian - Triassic boundary in the Bükk Mts., Hungary},
	url = {https://m2.mtmt.hu/api/publication/1339707},
	author = {Zajzon, Norbert and Szabó, Zs and Weiszburg, Tamás and Jeffries, T},
	doi = {10.1007/s00531-009-0500-y},
	journal-iso = {INT J EARTH SCI},
	journal = {INTERNATIONAL JOURNAL OF EARTH SCIENCES},
	volume = {100},
	unique-id = {1339707},
	issn = {1437-3254},
	year = {2011},
	eissn = {1437-3262},
	pages = {125-138},
	orcid-numbers = {Weiszburg, Tamás/0000-0001-8183-4434}
}

@article{MTMT:1447813,
	title = {A szélerózió szerepe a Dunántúl negyedidőszaki felszínfejlődésében.},
	url = {https://m2.mtmt.hu/api/publication/1447813},
	author = {Csillag, Gábor and Fodor, László and Sebe, Krisztina and Müller, P and Ruszkiczay-Rüdiger, Zsófia and Thamóné Bozsó, Edit and Bada, G},
	journal-iso = {FÖLDTANI KÖZLÖNY},
	journal = {FÖLDTANI KÖZLÖNY},
	volume = {140},
	unique-id = {1447813},
	issn = {0015-542X},
	year = {2010},
	eissn = {2559-902X},
	pages = {463-482},
	orcid-numbers = {Sebe, Krisztina/0000-0002-4647-2199}
}

@article{MTMT:1348919,
	title = {Sedimentology of a Permian playa lake: the Boda Claystone Formation, Hungary},
	url = {https://m2.mtmt.hu/api/publication/1348919},
	author = {Konrád, Gyula and Sebe, Krisztina and Halász, Amadé and Babinszki, Edit},
	doi = {10.2478/v10118-010-0002-1},
	journal-iso = {GEOLOGOS},
	journal = {GEOLOGOS},
	volume = {16},
	unique-id = {1348919},
	issn = {1426-8981},
	abstract = {The Upper Permian Boda Claystone Formation (BCF) in SW Hungary has been previously been identified as a saline lake deposit. A country-wide screening found this 800–1000 m thick succession the most suitable for the disposal of high-level radioactive waste in Hungary, and research into this formation has consequently been intensified since. The investigations included a detailed study of the sedimentological characteristics. Data obtained by mapping of the 25 km2 outcrop area of the formation and from more than 40 boreholes were processed. The sedimentary structures were investigated on outcrop to microscopic scales, and cycles in the succession were interpreted.
		The main lithofacies, sedimentary structures and ichnofossils are presented. They indicate that the major part of the succession was deposited in a playa mudflat and is not of lacustrine origin in a strict sense. The lake sediments are represented
		by laminated and ripple-marked/flaser-type cross-laminated claystones and siltstones and by massive dolomites;
		trace fossils include crawling traces and burrows. Partial or complete drying out of the lake commonly occurred after the formation of carbonate mud by evaporation. Periodic fluvial influx is recorded by cross-bedded sandstones and unsorted gravelly sandstones of up to pebble-sized angular grains. Fenestral and stromatolitic structures reflect the repeated appearance of playa mudflat conditions. The silty claystones, which compose the major part of the succession, lost their primary structures due to pedogenic processes and indicate prolonged subaerial intervals with soil formation and only ephemeral inundations. The presence of pedogenic carbonate concretions supports the interpretation of an arid climate and a relatively shallow groundwater table. Drying-out events shown by desiccation cracks and authigenic breccias can be traced all over the succession.
		The various facies form small-scale sedimentary cycles showing a shallowing-upward trend and the growing influence of aridity and subaerial exposure.},
	year = {2010},
	eissn = {2080-6574},
	pages = {27-41},
	orcid-numbers = {Sebe, Krisztina/0000-0002-4647-2199; Halász, Amadé/0000-0003-4582-8883}
}

@article{MTMT:1299028,
	title = {A felső-permi Cserdi Konglomerátum Formáció kavicsanyagának kőzettani és geokémiai vizsgálati eredményei (XV. szerkezetkutató fúrás, Ny-Mecsek)},
	url = {https://m2.mtmt.hu/api/publication/1299028},
	author = {Bodor, Sarolta and Szakmány, György},
	journal-iso = {FÖLDTANI KÖZLÖNY},
	journal = {FÖLDTANI KÖZLÖNY},
	volume = {139},
	unique-id = {1299028},
	issn = {0015-542X},
	year = {2009},
	eissn = {2559-902X},
	pages = {325-340},
	orcid-numbers = {Szakmány, György/0000-0002-9557-2030}
}

@article{MTMT:1337374,
	title = {A mecseki toarci feketepala Réka-völgyi szelvényének előzetes petrográfiai és nehézásvány-vizsgálati eredményei [The petrography and heavy minerals of the toarcian black shale of the réka valley section of the mecsek hills: A pilot study]},
	url = {https://m2.mtmt.hu/api/publication/1337374},
	author = {Raucsikné Varga, Andrea Beáta and Mikes, T and Raucsik, Béla},
	journal-iso = {FÖLDTANI KÖZLÖNY},
	journal = {FÖLDTANI KÖZLÖNY},
	volume = {139},
	unique-id = {1337374},
	issn = {0015-542X},
	year = {2009},
	eissn = {2559-902X},
	pages = {33-54},
	orcid-numbers = {Raucsikné Varga, Andrea Beáta/0000-0002-8673-1482; Raucsik, Béla/0000-0002-1951-5974}
}

@article{MTMT:1337379,
	title = {A felső-paleozoikumi Turonyi Formáció (Szlavóniai–Drávai-terrénum) pelites kőzeteinek ásványtani és kőzettani jellemzői [Mineralogical and petrological characteristics of mudrocks from the Upper Palaeozoic Turony Formation (Slavonia–Drava unit)]},
	url = {https://m2.mtmt.hu/api/publication/1337379},
	author = {Raucsikné Varga, Andrea Beáta and Raucsik, Béla and Kovácsné Kis, Viktória and Szakmány, György},
	journal-iso = {FÖLDTANI KÖZLÖNY},
	journal = {FÖLDTANI KÖZLÖNY},
	volume = {138},
	unique-id = {1337379},
	issn = {0015-542X},
	year = {2008},
	eissn = {2559-902X},
	pages = {5-20},
	orcid-numbers = {Raucsikné Varga, Andrea Beáta/0000-0002-8673-1482; Raucsik, Béla/0000-0002-1951-5974; Szakmány, György/0000-0002-9557-2030}
}

@{MTMT:1831361,
	title = {Complex examination of the Upper Paleozoic siliciclastic rocks from southern Transdanubia, SW Hungary - Mineralogical, petrographic, and geochemical study},
	url = {https://m2.mtmt.hu/api/publication/1831361},
	author = {Raucsikné Varga, Andrea Beáta and Szakmány, György and Árgyelán, T and Józsa, Sándor and Raucsik, Béla and Máthé, Zoltán},
	booktitle = {Sedimentary Provenance and Petrogenesis: Perspectives from Petrography and Geochemistry},
	doi = {10.1130/2006.2420(14)},
	unique-id = {1831361},
	year = {2007},
	pages = {221-240},
	orcid-numbers = {Raucsikné Varga, Andrea Beáta/0000-0002-8673-1482; Szakmány, György/0000-0002-9557-2030; Józsa, Sándor/0000-0001-8219-0044; Raucsik, Béla/0000-0002-1951-5974}
}

@inbook{MTMT:1834376,
	title = {The use of nummulitic chert in the Middle Palaeolithic in Hungary},
	url = {https://m2.mtmt.hu/api/publication/1834376},
	author = {Markó, András and Kázmér, Miklós},
	booktitle = {Die aktuellen Fragen des Mittelpaläolithikums in Mitteleuropa = Topical issues of the research of Middle Palaeolithic period in Central Europe},
	unique-id = {1834376},
	year = {2006},
	pages = {53-64},
	orcid-numbers = {Markó, András/0000-0002-7556-0091; Kázmér, Miklós/0000-0003-1092-1316}
}

@article{MTMT:1203520,
	title = {A Bodai Aleurolit Formáció törmelékes kőzettípusainak ásványtani, kőzettani és geokémiai jellemzői [Mineralogical, petrological and geochemical characteristics of the siliciclastic rock types of Boda Siltstone Formation]},
	url = {https://m2.mtmt.hu/api/publication/1203520},
	author = {Raucsikné Varga, Andrea Beáta and Raucsik, Béla and Szakmány, György and Máthé, Zoltán},
	journal-iso = {FÖLDTANI KÖZLÖNY},
	journal = {FÖLDTANI KÖZLÖNY},
	volume = {136},
	unique-id = {1203520},
	issn = {0015-542X},
	year = {2006},
	eissn = {2559-902X},
	pages = {201-231},
	orcid-numbers = {Raucsikné Varga, Andrea Beáta/0000-0002-8673-1482; Raucsik, Béla/0000-0002-1951-5974; Szakmány, György/0000-0002-9557-2030}
}

@article{MTMT:1303539,
	title = {Petrographic Investigation of Bronze and Iron Age Casting Moulds from the Collection of the Hungarian National Museum},
	url = {https://m2.mtmt.hu/api/publication/1303539},
	author = {Péterdi, Bálint and Kovács, T and Szakmány, György and T. Biró, Katalin},
	journal-iso = {GEOARCH BIOARCH STUD},
	journal = {GEOARCHAEOLOGICAL AND BIOARCHAEOLOGICAL STUDIES},
	volume = {3},
	unique-id = {1303539},
	issn = {1571-0750},
	year = {2005},
	pages = {87-90},
	orcid-numbers = {Szakmány, György/0000-0002-9557-2030}
}

@inbook{MTMT:1959646,
	title = {Bronzkori és vaskori öntőformák petrográfiai vizsgálata},
	url = {https://m2.mtmt.hu/api/publication/1959646},
	author = {Péterdi, Bálint},
	booktitle = {Momos III : "Fiatal Őskoros Kutatók" III. összejövetelének konferenciakötete: Halotkultusz és temetkezés},
	unique-id = {1959646},
	year = {2004},
	pages = {487-525}
}

@article{MTMT:1203502,
	title = {A Siklósbodony Sb-1 mélyfúrás feltételezett karbon-perm határképződményeinek ásványtani, kőzettani és geokémiai jellemzői [Mineralogical, petrographie and geochemical characteristics of siliciclastic rocks from the supposed Carboniferous-Permian boundary in borehole Siklósbodony Sb-1, South-western Hungary]},
	url = {https://m2.mtmt.hu/api/publication/1203502},
	author = {Raucsikné Varga, Andrea Beáta and Raucsik, Béla and Szakmány, György},
	journal-iso = {FÖLDTANI KÖZLÖNY},
	journal = {FÖLDTANI KÖZLÖNY},
	volume = {134},
	unique-id = {1203502},
	issn = {0015-542X},
	year = {2004},
	eissn = {2559-902X},
	pages = {321-343},
	orcid-numbers = {Raucsikné Varga, Andrea Beáta/0000-0002-8673-1482; Raucsik, Béla/0000-0002-1951-5974; Szakmány, György/0000-0002-9557-2030}
}

@article{MTMT:1302285,
	title = {Petrology and geochemistry of Upper Carboniferous siliciclastic rocks (Téseny Sandstone Formation) from the Slavonian-Drava Unit (Tisza Megaunit, S Hungary) - summarized results},
	url = {https://m2.mtmt.hu/api/publication/1302285},
	author = {Raucsikné Varga, Andrea Beáta and Szakmány, György and Józsa, Sándor and Máthé, Zoltán},
	doi = {10.1556/AGeol.46.2003.1.7},
	journal-iso = {ACTA GEOL HUNG},
	journal = {ACTA GEOLOGICA HUNGARICA: A QUARTERLY OF THE HUNGARIAN ACADEMY OF SCIENCES},
	volume = {46},
	unique-id = {1302285},
	issn = {0236-5278},
	year = {2003},
	pages = {95-113},
	orcid-numbers = {Raucsikné Varga, Andrea Beáta/0000-0002-8673-1482; Szakmány, György/0000-0002-9557-2030; Józsa, Sándor/0000-0001-8219-0044}
}

@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:1203436,
	title = {Eocén calcrete kavicsok a nyugat-mecseki miocén konglomerátumból [Eocene calcrete pebbles from Miocene conglomerate, Western Mecsek Mountains, Hungary]},
	url = {https://m2.mtmt.hu/api/publication/1203436},
	author = {Raucsikné Varga, Andrea Beáta and Szakmány, György and Raucsik, Béla and Kedves, M and Józsa, Sándor},
	journal-iso = {FÖLDTANI KÖZLÖNY},
	journal = {FÖLDTANI KÖZLÖNY},
	volume = {132},
	unique-id = {1203436},
	issn = {0015-542X},
	year = {2002},
	eissn = {2559-902X},
	pages = {57-82},
	orcid-numbers = {Raucsikné Varga, Andrea Beáta/0000-0002-8673-1482; Szakmány, György/0000-0002-9557-2030; Raucsik, Béla/0000-0002-1951-5974; Józsa, Sándor/0000-0001-8219-0044}
}

@article{MTMT:132558,
	title = {Petrographical, geochemical and geochronological constraints on igneous clasts and sediments hosted in the Oligo-Miocene Bakony Molasse, Hungary: evidence for a Paleo-Drava River system},
	url = {https://m2.mtmt.hu/api/publication/132558},
	author = {Benedek, K and Nagy, ZR and Dunkl, István and Szabó, Csaba and Józsa, Sándor},
	doi = {10.1007/s005310000183},
	journal-iso = {INT J EARTH SCI},
	journal = {INTERNATIONAL JOURNAL OF EARTH SCIENCES},
	volume = {90},
	unique-id = {132558},
	issn = {1437-3254},
	year = {2001},
	eissn = {1437-3262},
	pages = {519-533},
	orcid-numbers = {Szabó, Csaba/0000-0002-1580-6344; Józsa, Sándor/0000-0001-8219-0044}
}

@article{MTMT:1303024,
	title = {A nyugat-mecseki alsó-miocén konglomerátum karbon homokkő kavicsainak és a Tésenyi Homokkő Formáció képződményeinek petrográfiai és geokémiai összehasonlítása},
	url = {https://m2.mtmt.hu/api/publication/1303024},
	author = {Raucsikné Varga, Andrea Beáta and Szakmány, György and Józsa, Sándor and Máthé, Zoltán},
	journal-iso = {FÖLDTANI KÖZLÖNY},
	journal = {FÖLDTANI KÖZLÖNY},
	volume = {131},
	unique-id = {1303024},
	issn = {0015-542X},
	year = {2001},
	eissn = {2559-902X},
	pages = {11-36},
	orcid-numbers = {Raucsikné Varga, Andrea Beáta/0000-0002-8673-1482; Szakmány, György/0000-0002-9557-2030; Józsa, Sándor/0000-0001-8219-0044}
}

@article{MTMT:1302426,
	title = {An Upper Carboniferous-Lower Permian silicified wood in the Miocene conglomerate from the western Mecsek Mts. (southern Hungary)},
	url = {https://m2.mtmt.hu/api/publication/1302426},
	author = {Philippe, M and Szakmány, György and Gulyás-Kis, Cs and Józsa, Sándor},
	journal-iso = {NEUES JAHRB GEOL P-M},
	journal = {NEUES JAHRBUCH FUR GEOLOGIE UND PALAONTOLOGIE-MONATSHEFTE},
	volume = {2000},
	unique-id = {1302426},
	issn = {0028-3630},
	year = {2000},
	pages = {193-204},
	orcid-numbers = {Szakmány, György/0000-0002-9557-2030; Józsa, Sándor/0000-0001-8219-0044}
}

@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:1763183,
	title = {Interaction of basin-margin faults and tidal currents on nearshore sedimentary architecture and composition: A case study from the Early Miocene of northern Hungary},
	url = {https://m2.mtmt.hu/api/publication/1763183},
	author = {Sztanó, Orsolya and Józsa, Sándor},
	doi = {10.1016/S0040-1951(96)00196-5},
	journal-iso = {TECTONOPHYSICS},
	journal = {TECTONOPHYSICS},
	volume = {266},
	unique-id = {1763183},
	issn = {0040-1951},
	abstract = {The Darno Conglomerate and the Petervasara Sandstone with conglomeratic intercalations, both cropping out in northern Hungary, were formed along the eastern margin of the shallow Early Miocene sea within the Carpathian are. Ophiolite-derived elastic components in both formations indicate a close genetic relationship with each other and with the activity of the basin-margin Darno Fault, which seems to correspond with the coeval shoreline. The Darno Conglomerate was part of a small fault-controlled fan-delta supplying coarse clastics into the sea where the Petervasara Sandstone deposited. The conglomerates occur as small lobes interbedded within a field of tidally-driven sand waves. The coarse-grained clastics, which were admired to the main material of the sandstone, have been derived from Triassic-Jurassic ophiolite-related series (Meliata nappes) east of the Darno Fault. The composition of the lobes indicates that they were formed as small spit-like platforms attached to the fan-deltas of the Darno Conglomerate. As base level rose spits became drowned and their sediment was washed into the basin and reworked by the strong northward-directed tidal currents into elongated lobes 'mimicking' sand waves. A reduction in the amount of the less resistant pebble components of ophiolite-related origin and a relative enrichment of the resistant components towards the west indicate that pebbles had partly been transported in the offshore direction. The increasing rate of accumulation of ophiolite-derived heavy minerals and pebbles along the northern part of the coast indirectly suggests a contemporaneous left-lateral displacement along the basin-margin Darno Fault.},
	keywords = {MODEL; EVOLUTION; FAN-DELTA; pebble composition; fault-controlled delta; tidal currents; conglomerate},
	year = {1996},
	eissn = {1879-3266},
	pages = {319-341},
	orcid-numbers = {Sztanó, Orsolya/0000-0003-0786-3653; Józsa, Sándor/0000-0001-8219-0044}
}

@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:1763237,
	title = {Durvatörmelékes üledékek gravitációs tömegmozgásai egy gerecsei alsókréta tenger alatti csatornakitöltő konglomerátum példáján},
	url = {https://m2.mtmt.hu/api/publication/1763237},
	author = {Sztanó, Orsolya},
	journal-iso = {ÁLTALÁNOS FÖLDTANI SZEMLE},
	journal = {ÁLTALÁNOS FÖLDTANI SZEMLE},
	volume = {25},
	unique-id = {1763237},
	issn = {0133-6339},
	year = {1990},
	pages = {337-360},
	orcid-numbers = {Sztanó, Orsolya/0000-0003-0786-3653}
}

@article{MTMT:1131671,
	title = {A Maros- és a Körös-hordalék gránátjainak pásztázó-elektronmikroszkópos vizsgálata a hordalékkúpok kijelölése céljából},
	url = {https://m2.mtmt.hu/api/publication/1131671},
	author = {Polgári, Márta Piroska},
	journal-iso = {FÖLDTANI KÖZLÖNY},
	journal = {FÖLDTANI KÖZLÖNY},
	volume = {112},
	unique-id = {1131671},
	issn = {0015-542X},
	year = {1982},
	eissn = {2559-902X},
	pages = {143-160}
}