TY - CHAP AU - Horváth, Ferenc AU - Csontos, L AU - Cloetingh, S AU - Gerner, P AU - Dövényi, Péter ED - Wessely, G ED - Liebl, W TI - Compression during extension in the Pannonian Basin and its bearing on hydrocarbon exploration T2 - Oil and Gas in Alpidic Thrustbelts and Basins of Central and Eastern Europe PB - Geological Society of London CY - London SN - 189779973X T3 - EAGE Special Publication ; 5. PY - 1996 SP - 105 EP - 107 PG - 3 UR - https://m2.mtmt.hu/api/publication/1258208 ID - 1258208 LA - English DB - MTMT ER - TY - JOUR AU - Matyas, J AU - Burns, SJ AU - Muller, P AU - Magyar, Imre TI - What can stable isotopes say about salinity? An example from the late Miocene Pannonian Lake JF - PALAIOS J2 - PALAIOS VL - 11 PY - 1996 IS - 1 SP - 31 EP - 39 PG - 9 SN - 0883-1351 DO - 10.2307/3515114 UR - https://m2.mtmt.hu/api/publication/1890264 ID - 1890264 AB - The mid-to late Miocene ''Pannonian Lake'' was a primarily closed, saline lake which during its lifetime underwent a series of rapid salinity changes associated with faunal extinctions/radiations. The first two of these, at the Badenian/Sarmatian and Sarmatian/Pannonian boundaries signify the transition from a marine basin to a brackish lake and are marked by major faunal changes. The isotopic composition of molluscs from the lake, however, does not undergo major changes. The third transition, at the end of the Pannonian. and into the Pontian, is also marked by major faunal changes, thought initially to reflect further freshening of the lake. Both carbon, and oxygen isotope ratios of lake molluscs decrease by 4 to 6 parts per thousand at this transition. A consideration of salinity and oxygen. isotope mass balances for a closed or nearly-closed lake shows that major changes in salinity accompany relatively minor changes in water balance and isotopic composition. This result explains why the oxygen. isotope ratio of lake waters did not change during the initial freshening of the lake and suggests that the major isotopic changes observed later are not directly related to changes in the lake water balance which caused the salinity changes. The isotopic variations were driven mainly by other climatic factors, most likely changes in humidity and isotopic composition of inflow. 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 - Tóth, József TI - Hydraulic continuity in large sedimentary basins JF - HYDROGEOLOGY JOURNAL J2 - HYDROGEOL J VL - 3 PY - 1995 IS - 4 SP - 4 EP - 16 PG - 13 SN - 1431-2174 UR - https://m2.mtmt.hu/api/publication/2947503 ID - 2947503 LA - English DB - MTMT ER - TY - JOUR AU - Tari, Gábor AU - Báldi, T AU - Báldi-Beke, M TI - Paleogene retroarc flexural basin beneath the Neogene Pannonian Basin: A geodynamic model JF - TECTONOPHYSICS J2 - TECTONOPHYSICS VL - 226 PY - 1993 IS - 1-4 SP - 433 EP - 455 PG - 23 SN - 0040-1951 DO - 10.1016/0040-1951(93)90131-3 UR - https://m2.mtmt.hu/api/publication/22049448 ID - 22049448 N1 - Z9: 40 WC: Geochemistry & Geophysics LA - English DB - MTMT ER - TY - JOUR AU - Tari, Gábor AU - Horváth, Ferenc AU - RUMPLER, J TI - Styles of extension in the Pannonian Basin. JF - TECTONOPHYSICS J2 - TECTONOPHYSICS VL - 208 PY - 1992 IS - 1-3 SP - 203 EP - 219 PG - 17 SN - 0040-1951 DO - 10.1016/0040-1951(92)90345-7 UR - https://m2.mtmt.hu/api/publication/1255444 ID - 1255444 AB - Structural interpretation of reflection seismic profiles reveals distinct modes of upper crustal extension in the Pannonian Basin. While some subbasins in the Pannonian Basin complex show little extension (planar rotational normal faults), others are characterized by large magnitude of extension (detachment faults, metamorphic core complexes). Gravitational collapse of the Intra-Carpathian domain, combined with subduction zone roll-back is thought to be the driving mechanism of the Neogene back-arc extension. The very heterogeneously distributed extension is accommodated by transfer faults, which bound regions characterized by different polarity, direction, or amount of extension. In cross section these transfer faults are characterized by flower structures, typical for strike-slip faults. Seismic stratigraphic interpretations indicate that the non-marine post-rift sedimentary fill of the Pannonian Basin can be described in terms of sequence stratigraphy. The exceptionally good seismic sequence resolution allows recognition of third-order and also fourth-order depositional sequences, which may reflect the interplay of tectonics and eustasy, and Milankovitch scale climatic variations, respectively. LA - English DB - MTMT ER - TY - JOUR AU - M. Tóth, Tivadar TI - Origin of some minerals from the crystalline basement of Szeghalom, Eastern Hungary JF - ACTA MINERALOGICA PETROGRAPHICA J2 - ACTA MINERAL PETROGR VL - 32 PY - 1991 SP - 59 EP - 63 PG - 5 SN - 0365-8066 UR - https://m2.mtmt.hu/api/publication/1129785 ID - 1129785 LA - English 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 - AAPG 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 - TY - JOUR AU - ROYDEN, L AU - Horváth, Ferenc AU - RUMPLER, J TI - EVOLUTION OF THE PANNONIAN BASIN SYSTEM .1. TECTONICS JF - TECTONICS J2 - TECTONICS VL - 2 PY - 1983 IS - 1 SP - 63 EP - 90 PG - 28 SN - 0278-7407 DO - 10.1029/TC002i001p00063 UR - https://m2.mtmt.hu/api/publication/1255411 ID - 1255411 N1 - Cited By :193 Export Date: 29 June 2022 Correspondence Address: Royden, L. LA - English DB - MTMT ER - TY - JOUR AU - Tóth, József TI - A theoretical analysis of groundwater flow in small drainage basins JF - JOURNAL OF GEOPHYSICAL RESEARCH J2 - J GEOPHYS RES VL - 68 PY - 1963 IS - 10 SP - 4795 EP - 4812 PG - 18 SN - 0148-0227 UR - https://m2.mtmt.hu/api/publication/2947223 ID - 2947223 LA - English DB - MTMT ER -