@article{MTMT:31873512,
	title = {Source rock potential, crude oil characteristics and oil-to-source rock correlation in a Central Paratethys sub-basin, the Hungarian Palaeogene Basin (Pannonian Basin)},
	url = {https://m2.mtmt.hu/api/publication/31873512},
	author = {Körmös, Sándor and Sachsenhofer, Reinhard F. and Bechtel, Achim and Radovics, Balázs Géza and Milota, Katalin and Schubert, Félix},
	doi = {10.1016/j.marpetgeo.2021.104955},
	journal-iso = {MAR PETROL GEOL},
	journal = {MARINE AND PETROLEUM GEOLOGY},
	volume = {127},
	unique-id = {31873512},
	issn = {0264-8172},
	abstract = {Eocene and Lower Oligocene rocks are potential source rocks for crude oil accumulations in the Hungarian Palaeogene Basin. To enhance the understanding of the hydrocarbon system, this study (i) assesses the petroleum potential of Palaeogene formations, (ii) characterises the source rock facies of the accumulated oils, and (iii) provides an oil-to-source correlation. Rock-Eval data of samples from three boreholes (W?1, W?9 and W?12) show that most Palaeogene formations are mature at depths exceeding 2.1?2.5 km. The coal-bearing Kosd Formation includes good to excellent gas-(and oil-) prone source rocks. The overlying Buda Marl Formation is typically organic matter-lean but contains oil-prone rocks with up to 2.3 wt% TOC and a fair petroleum potential in borehole W?9. The Tard Clay Formation in W?12 reaches up to 1.9 wt% TOC and shows HI values up to 440 mg HC/g TOC, characterising the deposits as good petroleum source rocks. Based on low TOC contents, the Kiscell Clay Formation is not considered a source rock. Molecular parameters of 12 crude oil samples indicate a shaly source rock deposited in a marine/brackish environment. Salinity stratification, causing the development of oxygen-depleted conditions, is likely. The organic matter is dominated by aquatic biomass, including algae, dinoflagellates and chemoautotrophic bacteria. Minor angiosperm-dominated organic matter was transported into the basin from the shoreline. Specific V-shaped compound-specific carbon isotope patterns of n-alkanes observed in crude oils and extracts from the Tard Clay prove the dominant source rock. Minor differences between biomarker ratios are related to vertical and lateral facies variations within the Tard Clay Formation. The accumulated oils are slightly more mature than the Tard Clay in borehole W?12.},
	keywords = {Source rocks; CENTRAL PARATETHYS; Crude oil; Hungarian Palaeogene Basin; Oil-to-source rock correlation},
	year = {2021},
	eissn = {1873-4073},
	orcid-numbers = {Körmös, Sándor/0000-0003-4439-6804; Schubert, Félix/0000-0001-8647-5354}
}

@article{MTMT:31387995,
	title = {Petrographic and organic geochemical study of the Eocene Kosd Formation (northern Pannonian Basin). Implications for paleoenvironment and hydrocarbon source potential},
	url = {https://m2.mtmt.hu/api/publication/31387995},
	author = {Körmös, Sándor and Achim, Bechtel and Reinhard, F. Sachsenhofer and Radovics, Balázs Géza and Milota, Katalin and Schubert, Félix},
	doi = {10.1016/j.coal.2020.103555},
	journal-iso = {INT J COAL GEOL},
	journal = {INTERNATIONAL JOURNAL OF COAL GEOLOGY},
	volume = {228},
	unique-id = {31387995},
	issn = {0166-5162},
	year = {2020},
	eissn = {1872-7840},
	orcid-numbers = {Körmös, Sándor/0000-0003-4439-6804; Schubert, Félix/0000-0001-8647-5354}
}

@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}
}

@CONFERENCE{MTMT:31595923,
	title = {A magyar Paleogén-medence eocén tárolóinak kihívása - hatástanulmány},
	url = {https://m2.mtmt.hu/api/publication/31595923},
	author = {Radovics, Balázs Géza and Schubert, Félix},
	booktitle = {31st International Oil and Gas Conference and Exhibition, Siófok, Hungary},
	unique-id = {31595923},
	year = {2017},
	pages = {1},
	orcid-numbers = {Schubert, Félix/0000-0001-8647-5354}
}

@{MTMT:3265559,
	title = {A magyar paleogén medence szénhidrogén rendszere, és eocén tárolóinak kihívása - hatástanulmány},
	url = {https://m2.mtmt.hu/api/publication/3265559},
	author = {Radovics, Balázs Géza and Körmös, Sándor and Schubert, Félix},
	booktitle = {Ahol az elemek találkoznak: víz, föld és tűz határán},
	unique-id = {3265559},
	year = {2017},
	pages = {147-149},
	orcid-numbers = {Körmös, Sándor/0000-0003-4439-6804; Schubert, Félix/0000-0001-8647-5354}
}

@article{MTMT:26390889,
	title = {Petrologic comparison of the Gyod and Helesfa serpentinite bodies (Tisia Mega Unit, SW Hungary)},
	url = {https://m2.mtmt.hu/api/publication/26390889},
	author = {Kovacs, Gabor and Radovics, Balázs Géza and M. Tóth, Tivadar},
	doi = {10.3190/jgeosci.218},
	journal-iso = {J GEOSCI},
	journal = {JOURNAL OF GEOSCIENCES},
	volume = {61},
	unique-id = {26390889},
	issn = {1802-6222},
	year = {2016},
	eissn = {1803-1943},
	pages = {255-279},
	orcid-numbers = {M. Tóth, Tivadar/0000-0003-1012-1095}
}

@inproceedings{MTMT:31595932,
	title = {A Gyódi és Helesfai szerpentinit összehasonlító kőzettani vizsgálata (Tiszai Egység, D-Dunántúl) [Petrologic comparison of the Gyód and Helesfa serpentinite bodies (Tisza Unit, SW Hungary)]},
	url = {https://m2.mtmt.hu/api/publication/31595932},
	author = {Kovács, Gábor and M. Tóth, Tivadar and Radovics, Balázs Géza},
	booktitle = {IV. Kőzettani és Geokémiai Vándorgyűlés kiadványa : [Orfű, 2013. szeptember 12-14.]},
	unique-id = {31595932},
	year = {2013},
	pages = {16-20},
	orcid-numbers = {M. Tóth, Tivadar/0000-0003-1012-1095}
}