TY - JOUR AU - Szilaj, R AU - Szónoky, M AU - Geary, D H AU - Magyar, Imre AU - Müller, P TI - Stratigraphy, paleoecology, and paleogeography of the 'Congeria ungulacaprae beds' (Lymnocardium ponticum Zone) in NW Hungary: Study of the Daka outcrop JF - ACTA GEOLOGICA HUNGARICA: A QUARTERLY OF THE HUNGARIAN ACADEMY OF SCIENCES J2 - ACTA GEOL HUNG VL - 42 PY - 1999 IS - 1 SP - 33 EP - 55 PG - 23 SN - 0236-5278 UR - https://m2.mtmt.hu/api/publication/1890288 ID - 1890288 AB - The littoral 'Congeria ungulacaprae beds' (=Lymnocardium ponticum Zone) of the Late Miocene Lake Pannon are widely exposed around the Transdanubian Central Range of NW Hungary, especially on its NW side. Study of the mollusk fauna of the Daka outcrop, located near the classic locality of Kup, showed that the fauna of this zone represents a transitional stage between the older L. conjungens Zone and the younger L. decorum Zone. The characteristic mollusk association of the L. ponticum Zone is apparently missing from the stratigraphic record of the southern part of the Pannonian basin. This difference can be partly explained by the paleogeographical situation. The northwestern part of the basin, where the Daka fauna lived, was site of rapid delta progradation, whereas the southern shoreline lacked significant sediment input. However, the littoral, well-aerated, vegetation-rich environment represented by the Daka layers must have had its counterpart in the southern part of the basin, where its sediments were either eroded or lie covered by younger sediments in a more basinward position. The age of the Daka fauna and of the whole L. ponticum Zone is estimated between 9 and 10 Ma, on the basis of its correlation to magnetic polarity chron 4Ar in boreholes Berhida-3, Nagylozs-1, and Duka-II. LA - English DB - MTMT ER - TY - JOUR AU - Horváth, Ferenc TI - PHASES OF COMPRESSION DURING THE EVOLUTION OF THE PANNONIAN BASIN AND JF - MARINE AND PETROLEUM GEOLOGY J2 - MAR PETROL GEOL VL - 12 PY - 1995 IS - 8 SP - 837 EP - 844 PG - 8 SN - 0264-8172 DO - 10.1016/0264-8172(95)98851-U UR - https://m2.mtmt.hu/api/publication/1255453 ID - 1255453 N1 - DE: PANNONIAN BASIN; RIFTING; SEISMIC STRATIGRAPHY AB - Progress in understanding the structural evolution of the Pannonian Basin is reported. This has been driven by the application of seismic stratigraphy constrained by magnetostratigraphic data and the recent release of a great amount of hydrocarbon exploration data. This has led to a redefinition and better understanding of the syn-rift period and style of rifting. In addition, a complex structural evolution history during the post-rift phase has been recognized. Two compressive events are defined: one in the early stage and another in the late stage of evolution. The importance of these findings for hydrocarbon exploration includes an improved knowledge of the timing of trap formations and a possible explanation for remarkably variable reservoir pressures in pools of the Great Hungarian Plain. LA - English DB - MTMT ER - TY - JOUR AU - Magyar, Imre TI - Late Miocene mollusc biostratigraphy in the eastern part of the Pannonian Basin (Tiszantul, Hungary) JF - GEOLOGICA CARPATHICA J2 - GEOL CARPATH VL - 46 PY - 1995 IS - 1 SP - 29 EP - 36 PG - 8 SN - 1335-0552 UR - https://m2.mtmt.hu/api/publication/1890290 ID - 1890290 AB - Biostratigraphic study of Late Miocene (Pannonian and Pontian) endemic molluscs from east Hungarian part of the Pannonian Basin revealed the relative persistence of the deep water association during the Late Pannonian and Pontian. Consequently, the earlier interpretation of these forms as Pontian or Lower Pontian ones, and definition of the Early and Late Pontian substages by them, should be revised. The occurrences of the sublittoral association can be divided into two stratigraphic units. In the littoral facies zone 3 stratigraphic units were identified. Evolution from L. decorum to Prosodacnomya took place between 7.7 and 7.0 million years, according to magnetostratigraphic and seismic data. Basinward progradation is demonstrated by the geographic distribution of molluscs. -from Author LA - English DB - MTMT ER - TY - JOUR AU - Vakarcs, G. AU - P. R., Vail AU - Tari, Gábor AU - Pogácsás, György AU - R. E., Mattick AU - A., Szabó TI - 3RD-ORDER MIDDLE MIOCENE EARLY PLIOCENE DEPOSITIONAL SEQUENCES IN THE PROGRADING DELTA-COMPLEX OF THE PANNONIAN BASIN JF - TECTONOPHYSICS J2 - TECTONOPHYSICS VL - 240 PY - 1994 IS - 1-4 SP - 81 EP - 106 PG - 26 SN - 0040-1951 DO - 10.1016/0040-1951(94)90265-8 UR - https://m2.mtmt.hu/api/publication/2317242 ID - 2317242 N1 - Rice University, Dept. of Geology and Geophysics, Houston, TX 77251-1892, United States MOL RT Exploration Department, H-1039 Budapest, Hungary U.S. Geological Survey, Reston, VA 22092, United States Cited By :117 Export Date: 24 February 2023 Correspondence Address: Vakarcs, G.; Rice University, Dept. of Geology and Geophysics, Houston, TX 77251-1892, United States LA - English DB - MTMT ER - TY - JOUR AU - Pogácsás, György AU - Muller, P AU - Magyar, Imre TI - The role of seismic stratigraphy in understanding biological evolution in the Pannonian Lake (SE Europe, late Miocene) JF - GEOLOGIA CROATICA J2 - GEOL CROAT VL - 46 PY - 1993 IS - 1 SP - 63 EP - 69 PG - 7 SN - 1330-030X DO - 10.4154/GC.1993.05 UR - https://m2.mtmt.hu/api/publication/1890291 ID - 1890291 N1 - Nincs jelölve levelező szerzőség a közleményen. AB - The combined use of seismic stratigraphy and mollusc biostratigraphy in Late Neogene lacustrine deposits of the Pannonian basin offers three new approaches. First, the comparison of seismic facies and biofacies facilitates to make a distinction between biostratigraphic units and biofacies. Second, seismic datum levels permit crosschecking of discrete data, thus dating evolution events. Third, seismic monitoring of the sedimentary history of the basin helps in the understanding of the geographic distribution of molluscs. -Authors LA - English DB - MTMT ER - TY - JOUR AU - Kókay, J AU - Hámor, Tamás AU - Lantos, M AU - Müller, P TI - A Berhida-3. sz. fúrás paleomágneses és földtani vizsgálata JF - MAGYAR ÁLLAMI FÖLDTANI INTÉZET ÉVI JELENTÉSE J2 - M ÁLL FÖLDT INT JELENT VL - 1991 PY - 1991 SP - 45 EP - 63 PG - 19 SN - 0368-9751 UR - https://m2.mtmt.hu/api/publication/3322706 ID - 3322706 LA - Hungarian DB - MTMT ER - TY - CHAP AU - Horváth, Ferenc AU - Dovenyi, P AU - Szalay, A AU - Royden, LH ED - Royden, LH ED - Horváth, Ferenc TI - Subsidence; thermal; maturation history of the Great Hungarian Plain T2 - The Pannonian Basin: A Study in Basin Evolution/Book and Maps PB - American Association of Petroleum Geologists (AAPG) CY - Tulsa (OK) SN - 9780891813224 T3 - American Association of Petroleum Geologists Memoir, ISSN 0271-8529 ; 45. PY - 1988 SP - 355 EP - 372 PG - 18 UR - https://m2.mtmt.hu/api/publication/1256140 ID - 1256140 LA - English DB - MTMT ER -