TY - JOUR AU - Badics, B AU - Uhrin, András AU - Vető, István AU - Bartha, A AU - Sajgó, Csanád TI - Basin-centred gas in the makó trough, Hungary: A 3D basin and petroleum system modelling investigation JF - PETROLEUM GEOSCIENCE J2 - PETROL GEOSCI VL - 17 PY - 2011 IS - 4 SP - 405 EP - 416 PG - 12 SN - 1354-0793 DO - 10.1144/1354-079310-063 UR - https://m2.mtmt.hu/api/publication/1767727 ID - 1767727 N1 - Department of Applied Geology, Eötvös Loránd University of Sciences, Pázmány Péter street 1/C, H-1117 Budapest, Hungary Statoil, Grenseveien 21, Forushagen D4, N-4035 Stavanger, Norway Geological Institute of Hungary, Stefánia Street 14, H-1143 Budapest, Hungary Balogh Ádám Street 18/c, H-1026 Budapest, Hungary Schlumberger, 10001 Richmond Avenue, Houston, 77042 TX, United States Institute for Geochemical Research, Hungarian Academy of Sciences, 45 Budaörsi street, H-1112 Budapest, Hungary Cited By :10 Export Date: 24 February 2023 Correspondence Address: Badics, B.; Department of Applied Geology, Pázmány Péter street 1/C, H-1117 Budapest, Hungary; email: balb@statoil.com LA - English DB - MTMT ER - TY - JOUR AU - Szabó, B AU - Schubert, Félix AU - M. Tóth, Tivadar TI - Paleofluid evolution of the fractured basalt hydrocarbon reservoir in the Üllés–Ruzsa–Bordány area, SE Hungary JF - CENTRAL EUROPEAN GEOLOGY J2 - CENT EUR GEOL VL - 52 PY - 2009 IS - 3-4 SP - 299 EP - 323 PG - 25 SN - 1788-2281 DO - 10.1556/CEuGeol.52.2009.3-4.6 UR - https://m2.mtmt.hu/api/publication/1382753 ID - 1382753 LA - English DB - MTMT ER - TY - JOUR AU - Schubert, Félix AU - Diamond, L W AU - M. Tóth, Tivadar TI - Fluid-inclusion evidence of petroleum migration through a buried metamorphic dome in the Pannonian Basin, Hungary JF - CHEMICAL GEOLOGY J2 - CHEM GEOL VL - 244 PY - 2007 IS - 3-4 SP - 357 EP - 381 PG - 25 SN - 0009-2541 DO - 10.1016/j.chemgeo.2007.05.019 UR - https://m2.mtmt.hu/api/publication/1129827 ID - 1129827 LA - English DB - MTMT ER - TY - JOUR AU - Magyar, Imre AU - Juhász, Gy AU - Szuromi-Korecz, A AU - Sütő-Szentai, M TI - 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 JF - FÖLDTANI KÖZLÖNY J2 - FÖLDTANI KÖZLÖNY VL - 133 PY - 2004 SP - 521 EP - 540 PG - 20 SN - 0015-542X UR - https://m2.mtmt.hu/api/publication/1891351 ID - 1891351 LA - Hungarian DB - MTMT ER - TY - JOUR AU - Magyar, Imre AU - Geary, D H AU - Süto-Szentai, M AU - Lantos, M AU - Müller, P TI - Integrated biostratigraphic, magnetostratigraphic and chronostratigraphic correlations of the Late Miocene Lake Pannon deposits JF - ACTA GEOLOGICA HUNGARICA: A QUARTERLY OF THE HUNGARIAN ACADEMY OF SCIENCES J2 - ACTA GEOL HUNG VL - 42 PY - 1999 IS - 1 SP - 5 EP - 31 PG - 27 SN - 0236-5278 UR - https://m2.mtmt.hu/api/publication/1890285 ID - 1890285 N1 - Department of Geology and Geophysics, University of Wisconsin, Madison, WI, United States Geological Institute of Hungary, Budapest, Hungary Natural Historical Collection, Komló, Hungary 1215 W. Dayton Street, Madison, WI 53706, United States Városház tér 1, H-7300 Komló, Hungary Stefánia út 14, H-1143 Budapest, Hungary Cited By :94 Export Date: 24 February 2023 Correspondence Address: Magyar, I.; Department of Geology and Geophysics, 1215 W. Dayton Street, Madison, WI 53706, United States AB - 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. LA - English DB - MTMT ER -