@article{MTMT:1767727,
	title = {Basin-centred gas in the makó trough, Hungary: A 3D basin and petroleum system modelling investigation},
	url = {https://m2.mtmt.hu/api/publication/1767727},
	author = {Badics, B and Uhrin, András and Vető, István and Bartha, A and Sajgó, Csanád},
	doi = {10.1144/1354-079310-063},
	journal-iso = {PETROL GEOSCI},
	journal = {PETROLEUM GEOSCIENCE},
	volume = {17},
	unique-id = {1767727},
	issn = {1354-0793},
	year = {2011},
	eissn = {2041-496X},
	pages = {405-416}
}

@article{MTMT:1382753,
	title = {Paleofluid evolution of the fractured basalt hydrocarbon reservoir in the Üllés–Ruzsa–Bordány area, SE Hungary},
	url = {https://m2.mtmt.hu/api/publication/1382753},
	author = {Szabó, B and Schubert, Félix and M. Tóth, Tivadar},
	doi = {10.1556/CEuGeol.52.2009.3-4.6},
	journal-iso = {CENT EUR GEOL},
	journal = {CENTRAL EUROPEAN GEOLOGY},
	volume = {52},
	unique-id = {1382753},
	issn = {1788-2281},
	year = {2009},
	eissn = {1789-3348},
	pages = {299-323},
	orcid-numbers = {Schubert, Félix/0000-0001-8647-5354; 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:1891351,
	title = {A pannóniai Tótkomlósi Mészmárga Tagozat kifejlődése és kora a Battonya-pusztaföldvári-hátság környezetében. The Tótkomlós Calcareous Marl Member of the Lake Pannon sedimentary sequence in the Battonya-Pusztaföldvár region, SE Hungary},
	url = {https://m2.mtmt.hu/api/publication/1891351},
	author = {Magyar, Imre and Juhász, Gy and Szuromi-Korecz, A and Sütő-Szentai, M},
	journal-iso = {FÖLDTANI KÖZLÖNY},
	journal = {FÖLDTANI KÖZLÖNY},
	volume = {133},
	unique-id = {1891351},
	issn = {0015-542X},
	year = {2004},
	eissn = {2559-902X},
	pages = {521-540}
}

@article{MTMT:1890285,
	title = {Integrated biostratigraphic, magnetostratigraphic and chronostratigraphic correlations of the Late Miocene Lake Pannon deposits},
	url = {https://m2.mtmt.hu/api/publication/1890285},
	author = {Magyar, Imre and Geary, D H and Süto-Szentai, M and Lantos, M and Müller, P},
	journal-iso = {ACTA GEOL HUNG},
	journal = {ACTA GEOLOGICA HUNGARICA: A QUARTERLY OF THE HUNGARIAN ACADEMY OF SCIENCES},
	volume = {42},
	unique-id = {1890285},
	issn = {0236-5278},
	abstract = {Due to the highly endemic nature of the Late Miocene Lake Pannon's aquatic biota, the stratigraphic correlation of the lake's sediments with the global chronostratigraphic system is dependent upon mammal biostratigraphy, magnetostratigraphy, and radio-isotopic age determinations. However, correlation of mammal localities and isotopically dated volcanic formations with the lacustrine sequence is possible only in a few instances, offering limited independent data for magnetostratigraphic interpretation. In this paper we construct a correlation chart that integrates biostratigraphy (dinoflagellates and mollusks) with the results of physical dating methods. The average time resolution of our biozones (excluding deep-water mollusk zones) is 1 Ma. There is a difference, however, in the amount of available data and consequently in the reliability of our correlations between the lower (older than approximately 9.5 Ma) and upper parts of the sedimentary sequence; the former is well-established, whereas a scarcity of radio-isotopic ages from the upper part of the sequence results in more uncertainty. In addition, a biostratigraphic subdivision of the last ca. 3 Ma interval of the lacustrine sequence is almost entirely lacking. The only opportunity for interbasinal biostratigraphic correlation within the lifetime of Lake Pannon is the Early Pontian migration event, when a great number of the Lake Pannon endemic species entered the Eastern Paratethys. However, due to the scarcity of chronological data from the Late Miocene of the respective basins, correlation of the Eastern Paratethyan Pontian Stage to the Lake Pannon deposits carriers at least a 1.3 Ma uncertainty.},
	keywords = {Hungary; biostratigraphy; Pannonian Basin; Neogene; Miocene; Lake Pannon; Paratethys; paleolimnology; Chronostratigraphy; magnetostratigraphy; extinct lakes; lake evolution},
	year = {1999},
	pages = {5-31}
}