@article{MTMT:1890288, title = {Stratigraphy, paleoecology, and paleogeography of the 'Congeria ungulacaprae beds' (Lymnocardium ponticum Zone) in NW Hungary: Study of the Daka outcrop}, url = {https://m2.mtmt.hu/api/publication/1890288}, author = {Szilaj, R and Szónoky, M and Geary, D H and Magyar, Imre and Müller, P}, journal-iso = {ACTA GEOL HUNG}, journal = {ACTA GEOLOGICA HUNGARICA: A QUARTERLY OF THE HUNGARIAN ACADEMY OF SCIENCES}, volume = {42}, unique-id = {1890288}, issn = {0236-5278}, abstract = {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.}, keywords = {Hungary; Mollusca; biostratigraphy; STRATIGRAPHY; Pannonian Basin; Neogene; Miocene; paleogeography; paleoecology; Lake Pannon; mollusc; paleolimnology; extinct lakes; Transdanubian Central Range; lake evolution}, year = {1999}, pages = {33-55} } @article{MTMT:1255453, title = {PHASES OF COMPRESSION DURING THE EVOLUTION OF THE PANNONIAN BASIN AND}, url = {https://m2.mtmt.hu/api/publication/1255453}, author = {Horváth, Ferenc}, doi = {10.1016/0264-8172(95)98851-U}, journal-iso = {MAR PETROL GEOL}, journal = {MARINE AND PETROLEUM GEOLOGY}, volume = {12}, unique-id = {1255453}, issn = {0264-8172}, abstract = {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.}, year = {1995}, eissn = {1873-4073}, pages = {837-844} } @article{MTMT:1890290, title = {Late Miocene mollusc biostratigraphy in the eastern part of the Pannonian Basin (Tiszantul, Hungary)}, url = {https://m2.mtmt.hu/api/publication/1890290}, author = {Magyar, Imre}, journal-iso = {GEOL CARPATH}, journal = {GEOLOGICA CARPATHICA}, volume = {46}, unique-id = {1890290}, issn = {1335-0552}, abstract = {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}, keywords = {biostratigraphy; Miocene; palaeobiogeography; mollusc; Pannonian; Hungary, Tiszantul, Pannonian Basin; Pontian}, year = {1995}, eissn = {1336-8052}, pages = {29-36} } @article{MTMT:2317242, title = {3RD-ORDER MIDDLE MIOCENE EARLY PLIOCENE DEPOSITIONAL SEQUENCES IN THE PROGRADING DELTA-COMPLEX OF THE PANNONIAN BASIN}, url = {https://m2.mtmt.hu/api/publication/2317242}, author = {Vakarcs, G. and P. R., Vail and Tari, Gábor and Pogácsás, György and R. E., Mattick and A., Szabó}, doi = {10.1016/0040-1951(94)90265-8}, journal-iso = {TECTONOPHYSICS}, journal = {TECTONOPHYSICS}, volume = {240}, unique-id = {2317242}, issn = {0040-1951}, year = {1994}, eissn = {1879-3266}, pages = {81-106} } @article{MTMT:1890291, title = {The role of seismic stratigraphy in understanding biological evolution in the Pannonian Lake (SE Europe, late Miocene)}, url = {https://m2.mtmt.hu/api/publication/1890291}, author = {Pogácsás, György and Muller, P and Magyar, Imre}, doi = {10.4154/GC.1993.05}, journal-iso = {GEOL CROAT}, journal = {GEOLOGIA CROATICA}, volume = {46}, unique-id = {1890291}, issn = {1330-030X}, abstract = {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}, keywords = {biostratigraphy; Miocene; Europe, Pannonian Basin; sedimentary basin; mollusc; seismic stratigraphy}, year = {1993}, eissn = {1333-4875}, pages = {63-69} } @article{MTMT:3322706, title = {A Berhida-3. sz. fúrás paleomágneses és földtani vizsgálata}, url = {https://m2.mtmt.hu/api/publication/3322706}, author = {Kókay, J and Hámor, Tamás and Lantos, M and Müller, P}, journal-iso = {M ÁLL FÖLDT INT JELENT}, journal = {MAGYAR ÁLLAMI FÖLDTANI INTÉZET ÉVI JELENTÉSE}, volume = {1991}, unique-id = {3322706}, issn = {0368-9751}, year = {1991}, pages = {45-63} } @inbook{MTMT:1256140, title = {Subsidence; thermal; maturation history of the Great Hungarian Plain}, url = {https://m2.mtmt.hu/api/publication/1256140}, author = {Horváth, Ferenc and Dovenyi, P and Szalay, A and Royden, LH}, booktitle = {The Pannonian Basin: A Study in Basin Evolution/Book and Maps}, unique-id = {1256140}, year = {1988}, pages = {355-372} }