TY - JOUR AU - M. Tóth, Tivadar AU - Vargáné Tóth, I TI - Lithologically controlled behaviour of the Dorozsma metamorphic hydrocarbon reservoir (Pannonian Basin, SE Hungary) JF - JOURNAL OF PETROLEUM SCIENCE AND ENGINEERING J2 - J PETROL SCI ENG VL - 195 PY - 2020 PG - 16 SN - 0920-4105 DO - 10.1016/j.petrol.2020.107748 UR - https://m2.mtmt.hu/api/publication/31614407 ID - 31614407 N1 - Cited By :1 Export Date: 12 February 2021 Correspondence Address: M Tóth, T.; University of Szeged, Hungary; email: mtoth@geo.u-szeged.hu Funding text 1: The authors thank Enago (www.enago.com) for the English language review. Three anonymous reviewers are thanked for their valuable comments. Cited By :3 Export Date: 12 September 2021 Correspondence Address: M Tóth, T.; University of Szeged, Hungary; email: mtoth@geo.u-szeged.hu LA - English DB - MTMT ER - TY - JOUR AU - M. Tóth, Tivadar AU - Schubert, Félix TI - Evolution of the arc-derived orthogneiss recorded in exotic xenoliths of the Koros Complex (Tisza Megaunit, SE Hungary) JF - JOURNAL OF GEOSCIENCES J2 - J GEOSCI VL - 63 PY - 2018 IS - 1 SP - 21 EP - 46 PG - 26 SN - 1802-6222 DO - 10.3190/jgeosci.253 UR - https://m2.mtmt.hu/api/publication/27569302 ID - 27569302 N1 - Funding Agency and Grant Number: Schweizerische NationalfondsSwiss National Science Foundation (SNSF) [21-26579.89] Funding text: The co-operation and discussion with J. Zachar is acknowledged. The electron microprobe laboratory at the University of Bern was sponsored by the Schweizerische Nationalfonds (No.: 21-26579.89). Thorough reviews of Prokop Zavada, Martin Racek and an anonymous reviewer are thanked. P. Hasalova is acknowledged for her editorial work on the manuscript. Cited By :1 Export Date: 11 February 2021 Correspondence Address: Tóth, T.M.; Department of Mineralogy, Egyetem str. 2-6, Hungary; email: mtoth@geo.u-szeged.hu Funding details: Universität Bern, Ub, 21-26579.89 Funding text 1: The co-operation and discussion with J. Zachar is acknowledged. The electron microprobe laboratory at the University of Bern was sponsored by the Schweizerische Nationalfonds (No.: 21-26579.89). Thorough reviews of Prokop Závada, Martin Racek and an anonymous reviewer are thanked. P. Hasalová is acknowledged for her editorial work on the manuscript. Funding text 2: Acknowledgements. The co-operation and discussion with J. Zachar is acknowledged. The electron microprobe laboratory at the University of Bern was sponsored by the Schweizerische Nationalfonds (No.: 21-26579.89). Thorough reviews of Prokop Závada, Martin Racek and an anonymous reviewer are thanked. P. Hasalová is acknowledged for her editorial work on the manuscript. Cited By :1 Export Date: 12 February 2021 Correspondence Address: Tóth, T.M.; Department of Mineralogy, Egyetem str. 2-6, Hungary; email: mtoth@geo.u-szeged.hu Funding details: Universität Bern, Ub, 21-26579.89 Funding text 1: The co-operation and discussion with J. Zachar is acknowledged. The electron microprobe laboratory at the University of Bern was sponsored by the Schweizerische Nationalfonds (No.: 21-26579.89). Thorough reviews of Prokop Závada, Martin Racek and an anonymous reviewer are thanked. P. Hasalová is acknowledged for her editorial work on the manuscript. Funding text 2: Acknowledgements. The co-operation and discussion with J. Zachar is acknowledged. The electron microprobe laboratory at the University of Bern was sponsored by the Schweizerische Nationalfonds (No.: 21-26579.89). Thorough reviews of Prokop Závada, Martin Racek and an anonymous reviewer are thanked. P. Hasalová is acknowledged for her editorial work on the manuscript. Cited By :3 Export Date: 12 September 2021 Correspondence Address: Tóth, T.M.; Department of Mineralogy, Egyetem str. 2-6, Hungary; email: mtoth@geo.u-szeged.hu Funding details: Universität Bern, Ub, 21-26579.89 Funding text 1: The co-operation and discussion with J. Zachar is acknowledged. The electron microprobe laboratory at the University of Bern was sponsored by the Schweizerische Nationalfonds (No.: 21-26579.89). Thorough reviews of Prokop Závada, Martin Racek and an anonymous reviewer are thanked. P. Hasalová is acknowledged for her editorial work on the manuscript. Funding text 2: Acknowledgements. The co-operation and discussion with J. Zachar is acknowledged. The electron microprobe laboratory at the University of Bern was sponsored by the Schweizerische Nationalfonds (No.: 21-26579.89). Thorough reviews of Prokop Závada, Martin Racek and an anonymous reviewer are thanked. P. Hasalová is acknowledged for her editorial work on the manuscript. LA - English DB - MTMT ER - TY - JOUR AU - Papp, Nikoletta AU - Raucsikné Varga, Andrea Beáta AU - Mészáros, Előd AU - Raucsik, Béla TI - A dorozsmai márvány (Tiszai-főegység) kőzettani újravizsgálata: deformáció és fluidum hatása a mikroszerkezet fejlődésére JF - FÖLDTANI KÖZLÖNY J2 - FÖLDTANI KÖZLÖNY VL - 147 PY - 2017 IS - 4 SP - 337 EP - 356 PG - 19 SN - 0015-542X DO - 10.23928/foldt.kozl.2017.147.4.337 UR - https://m2.mtmt.hu/api/publication/3304112 ID - 3304112 N1 - Cited By :4 Export Date: 26 August 2022 Correspondence Address: Papp, N.; SZTE TTIK Ásványtani, Egyetem utca 2, Hungary; email: pappnicki@gmail.com LA - Hungarian DB - MTMT ER - TY - JOUR AU - Molnár, L AU - M. Tóth, Tivadar AU - Schubert, Félix TI - Structural controls on petroleum migration and entrapment within the faulted basement blocks of Szeghalom Dome (Pannonian Basin, SE Hungary) JF - GEOLOGIA CROATICA J2 - GEOL CROAT VL - 68 PY - 2015 IS - 3 SP - 247 EP - 259 PG - 14 SN - 1330-030X DO - 10.4154/gc.2015.19 UR - https://m2.mtmt.hu/api/publication/2949635 ID - 2949635 N1 - Funding Agency and Grant Number: research Balazs KISS (MOL) Funding text: We thank MOL Hungarian Oil and Gas Company for providing the samples, datasets and the financial support of this research Balazs KISS (MOL) is thanked for the fruitful discussions about the behaviour of the Szeghalom reservoir. Reviews by Istvan BERCZI and Gyula MAROS have significantly improved the manuscript, and are much appreciated. English was corrected by American Journal Experts. Cited By :5 Export Date: 11 February 2021 Cited By :5 Export Date: 12 February 2021 Cited By :6 Export Date: 12 September 2021 LA - English DB - MTMT ER - TY - JOUR AU - Fiser-Nagy, Ágnes AU - Varga-Tóth, I AU - M. Tóth, Tivadar TI - Lithology identification using open-hole well-log data in the metamorphic Kiskunhalas-NE hydrocarbon reservoir, South Hungary JF - ACTA GEODAETICA ET GEOPHYSICA J2 - ACTA GEOD GEOPHYS VL - 49 PY - 2014 IS - 1 SP - 57 EP - 78 PG - 22 SN - 2213-5812 DO - 10.1007/s40328-013-0037-1 UR - https://m2.mtmt.hu/api/publication/2474978 ID - 2474978 AB - in press LA - English DB - MTMT ER - TY - JOUR AU - Fiser-Nagy, Ágnes AU - M. Tóth, Tivadar AU - Vásárhelyi, Balázs AU - Földes, Tamás TI - Integrated core study of a fractured metamorphic HC-reservoir; Kiskunhalas-NE, Pannonian Basin JF - ACTA GEODAETICA ET GEOPHYSICA J2 - ACTA GEOD GEOPHYS VL - 48 PY - 2013 IS - 1 SP - 53 EP - 75 PG - 23 SN - 2213-5812 DO - 10.1007/s40328-012-0008-y UR - https://m2.mtmt.hu/api/publication/2190426 ID - 2190426 N1 - Funding Agency and Grant Number: European UnionEuropean Union (EU); European Social FundEuropean Social Fund (ESF); [TAMOP-4.2.2/B-10/1-2010-0012] Funding text: We thank MOL Hungarian Oil and Gas Company for making the study of the samples and thin sections possible. Balazs Kiss is thanked for the fruitful discussions about the behaviour of the KIHANE reservoir. The publication is supported by the European Union and co-funded by the European Social Fund. Project title: "Broadening the knowledge base and supporting the long term professional sustainability of the Research University Centre of Excellence at the University of Szeged by ensuring the rising generation of excellent scientists". Project number: TAMOP-4.2.2/B-10/1-2010-0012. English was corrected by Proof-Reading-Service.com. Department of Mineralogy Geochemistry and Petrology, University of Szeged, P.O. Box 651, 6701 Szeged, Hungary Department of Structural Engineering, Pollack Mihály Faculty of Engineering, University of Pécs, Pécs, Hungary Institute of Diagnostic Imaging and Radiation Oncology, Kaposvár University, Kaposvár, Hungary Cited By :1 Export Date: 11 February 2021 Correspondence Address: Nagy, A.; Department of Mineralogy Geochemistry and Petrology, P.O. Box 651, 6701 Szeged, Hungary; email: agnes.nagy@geo.u-szeged.hu Funding details: European Social Fund, ESF Funding details: European Commission, EC Funding text 1: Acknowledgements We thank MOL Hungarian Oil and Gas Company for making the study of the samples and thin sections possible. Balázs Kiss is thanked for the fruitful discussions about the behaviour of the KIHA-NE reservoir. The publication is supported by the European Union and co-funded by the European Social Fund. Project title: “Broadening the knowledge base and supporting the long term professional sustainability of the Research University Centre of Excellence at the University of Szeged by ensuring the rising generation of excellent scientists”. Project number: TÁMOP-4.2.2/B-10/1-2010-0012. English was corrected by ProofReading-Service.com. Department of Mineralogy Geochemistry and Petrology, University of Szeged, P.O. Box 651, 6701 Szeged, Hungary Department of Structural Engineering, Pollack Mihály Faculty of Engineering, University of Pécs, Pécs, Hungary Institute of Diagnostic Imaging and Radiation Oncology, Kaposvár University, Kaposvár, Hungary Cited By :1 Export Date: 12 February 2021 Correspondence Address: Nagy, A.; Department of Mineralogy Geochemistry and Petrology, P.O. Box 651, 6701 Szeged, Hungary; email: agnes.nagy@geo.u-szeged.hu Funding details: European Social Fund, ESF Funding details: European Commission, EC Funding text 1: Acknowledgements We thank MOL Hungarian Oil and Gas Company for making the study of the samples and thin sections possible. Balázs Kiss is thanked for the fruitful discussions about the behaviour of the KIHA-NE reservoir. The publication is supported by the European Union and co-funded by the European Social Fund. Project title: “Broadening the knowledge base and supporting the long term professional sustainability of the Research University Centre of Excellence at the University of Szeged by ensuring the rising generation of excellent scientists”. Project number: TÁMOP-4.2.2/B-10/1-2010-0012. English was corrected by ProofReading-Service.com. Department of Mineralogy Geochemistry and Petrology, University of Szeged, P.O. Box 651, 6701 Szeged, Hungary Department of Structural Engineering, Pollack Mihály Faculty of Engineering, University of Pécs, Pécs, Hungary Institute of Diagnostic Imaging and Radiation Oncology, Kaposvár University, Kaposvár, Hungary Cited By :3 Export Date: 12 September 2021 Correspondence Address: Nagy, A.; Department of Mineralogy Geochemistry and Petrology, P.O. Box 651, 6701 Szeged, Hungary; email: agnes.nagy@geo.u-szeged.hu Funding details: European Commission, EC Funding details: European Social Fund, ESF Funding text 1: Acknowledgements We thank MOL Hungarian Oil and Gas Company for making the study of the samples and thin sections possible. Balázs Kiss is thanked for the fruitful discussions about the behaviour of the KIHA-NE reservoir. The publication is supported by the European Union and co-funded by the European Social Fund. Project title: “Broadening the knowledge base and supporting the long term professional sustainability of the Research University Centre of Excellence at the University of Szeged by ensuring the rising generation of excellent scientists”. Project number: TÁMOP-4.2.2/B-10/1-2010-0012. English was corrected by ProofReading-Service.com. LA - English DB - MTMT ER - TY - JOUR AU - Buda, György AU - Pál-Molnár, Elemér AU - Koller, F TI - Mafic enclaves in peraluminous Variscan granitoid in the Battonya Unit from Southeast Hungary JF - GEOLOGIA CROATICA J2 - GEOL CROAT VL - 65 PY - 2012 IS - 2 SP - 243 EP - 253 PG - 11 SN - 1330-030X DO - 10.4154/GC.2012.15 UR - https://m2.mtmt.hu/api/publication/2011063 ID - 2011063 N1 - Funding Agency and Grant Number: Hungarian National Research Fund (OTKA) [K-67787] Funding text: The project was supported by the Hungarian National Research Fund (OTKA), No: K-67787. LA - English DB - MTMT ER - TY - JOUR AU - Fiser-Nagy, Ágnes AU - M. Tóth, Tivadar TI - Petrology and tectonic evolution of the Kiskunhalas-NE fractured hydrocarbon reservoir, South Hungary JF - CENTRAL EUROPEAN GEOLOGY J2 - CENT EUR GEOL VL - 55 PY - 2012 IS - 1 SP - 1 EP - 22 PG - 22 SN - 1788-2281 DO - 10.1556/CEuGeol.55.2012.1.1 UR - https://m2.mtmt.hu/api/publication/1843346 ID - 1843346 N1 - Cited By :6 Export Date: 12 February 2021 Correspondence Address: Nagy, A.; University of Szeged, , Szeged, Hungary LA - English DB - MTMT ER - TY - CHAP AU - Balogh, K AU - M. Tóth, Tivadar AU - Dunkl, István AU - Scherrer, N ED - M. Tóth, Tivadar TI - A polimetamorf aljzat geokronológiai viszonyai a Szeghalom és a Mezősas-Furta háton T2 - Magmás és metamorf képződmények a Tiszai Egységben PB - SZTE TTIK Földrajzi és Földtani Tanszékcsoport CY - Szeged SN - 9789634829782 T3 - GeoLitera, ISSN 2060-7067 PY - 2009 SP - 147 EP - 160 PG - 14 UR - https://m2.mtmt.hu/api/publication/1348928 ID - 1348928 LA - Hungarian DB - MTMT ER - TY - CHAP AU - Zachar, J AU - M. Tóth, Tivadar ED - M. Tóth, Tivadar TI - A Jánoshalma eklogit petrológiája T2 - Magmás és metamorf képződmények a Tiszai Egységben PB - SZTE TTIK Földrajzi és Földtani Tanszékcsoport CY - Szeged SN - 9789634829782 T3 - GeoLitera, ISSN 2060-7067 PY - 2009 SP - 117 EP - 144 PG - 28 UR - https://m2.mtmt.hu/api/publication/1382756 ID - 1382756 LA - Hungarian DB - MTMT ER - TY - JOUR AU - M. Tóth, Tivadar AU - Redlerné, Tátrai M AU - Kummer, I TI - A Szeghalom környéki metamorf aljzat kiemelkedés szerkezetfejlődése és felépítése kőzettani és szeizmikus adatok alapján [Structural evolution of the Szeghalom metamorphic dome on the basis of petrological and seismic data] JF - MAGYAR GEOFIZIKA J2 - MAGYAR GEOFIZIKA VL - 49 PY - 2008 IS - 4 SP - 143 EP - 151 PG - 9 SN - 0025-0120 UR - https://m2.mtmt.hu/api/publication/1348922 ID - 1348922 N1 - Szegedi Tudományegyetem Ásványtani, Geokémiai és Kozettani Tanszék, H-6722 Szeged, Egyetem u. 2 Magyar Állami Eötvös Loránd Geofizikai Intézet, H-1145 Budapest, Kolumbusz u. 17-23 Cited By :2 Export Date: 12 February 2021 Correspondence Address: Tivadar, M. T.; Szegedi Tudományegyetem Ásványtani, , H-6722 Szeged, Egyetem u. 2; email: mtoth@geo.u-szeged.hu Szegedi Tudományegyetem Ásványtani, Geokémiai és Kozettani Tanszék, H-6722 Szeged, Egyetem u. 2 Magyar Állami Eötvös Loránd Geofizikai Intézet, H-1145 Budapest, Kolumbusz u. 17-23 Cited By :3 Export Date: 12 September 2021 Correspondence Address: Tivadar, M. T.; Szegedi Tudományegyetem Ásványtani, , H-6722 Szeged, Egyetem u. 2; email: mtoth@geo.u-szeged.hu LA - Hungarian DB - MTMT ER - TY - THES AU - M. Tóth, Tivadar TI - Repedezett, metamorf fluidumtárolók az Alföld aljazatában PY - 2008 UR - https://m2.mtmt.hu/api/publication/30931322 ID - 30931322 LA - Hungarian 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 - Zachar, J AU - M. Tóth, Tivadar AU - Janák, M TI - Kyanite eclogite xenolith from the orthogneiss terrane of the Tisza Megaunit, Jánoshalma area, crystalline basement of southern Hungary JF - LITHOS J2 - LITHOS VL - 99 PY - 2007 IS - 3-4 SP - 249 EP - 265 PG - 17 SN - 0024-4937 DO - 10.1016/j.lithos.2007.06.001 UR - https://m2.mtmt.hu/api/publication/1129826 ID - 1129826 LA - English DB - MTMT ER - TY - JOUR AU - M. Tóth, Tivadar AU - Zachar, J TI - Petrology and deformation history of the metamorphic basement in the Mezősas-Furta crystalline high (SE Hungary) JF - ACTA GEOLOGICA HUNGARICA: A QUARTERLY OF THE HUNGARIAN ACADEMY OF SCIENCES J2 - ACTA GEOL HUNG VL - 49 PY - 2006 IS - 2 SP - 165 EP - 188 PG - 24 SN - 0236-5278 DO - 10.1556/AGeol.49.2006.2.4 UR - https://m2.mtmt.hu/api/publication/1129819 ID - 1129819 LA - English DB - MTMT ER - TY - JOUR AU - Pál-Molnár, Elemér AU - Lelkes-Felvári, Gy AU - Batki, Anikó AU - Sassi, R TI - Metamorphic petrology and geochemistry of the Sarkadkeresztúr Basement-High with special regard to orthogneiss (Tisza Mega-unit, SE Hungary) JF - ACTA GEOLOGICA HUNGARICA: A QUARTERLY OF THE HUNGARIAN ACADEMY OF SCIENCES J2 - ACTA GEOL HUNG VL - 48 PY - 2005 IS - 4 SP - 395 EP - 418 PG - 24 SN - 0236-5278 DO - 10.1556/AGeol.48.2005.4.3 UR - https://m2.mtmt.hu/api/publication/1132980 ID - 1132980 LA - English DB - MTMT ER - TY - JOUR AU - Zachar, J AU - M. Tóth, Tivadar TI - Petrology of the metamorphic basement of the Tisza block at the Jánoshalma high, S Hungary JF - ACTA GEOLOGICA HUNGARICA: A QUARTERLY OF THE HUNGARIAN ACADEMY OF SCIENCES J2 - ACTA GEOL HUNG VL - 47 PY - 2004 IS - 4 SP - 349 EP - 371 PG - 23 SN - 0236-5278 DO - 10.1556/AGeol.47.2004.4.3 UR - https://m2.mtmt.hu/api/publication/1129817 ID - 1129817 LA - English DB - MTMT ER - TY - JOUR AU - M. Tóth, Tivadar AU - Kedves, M AU - Schubert, Félix TI - Az Alföld metamorf aljzatának exhumációja a Szeghalom-dóm területén: palinológiai bizonyítékok JF - FÖLDTANI KÖZLÖNY J2 - FÖLDTANI KÖZLÖNY VL - 133 PY - 2003 IS - 4 SP - 547 EP - 562 PG - 16 SN - 0015-542X UR - https://m2.mtmt.hu/api/publication/1129812 ID - 1129812 LA - Hungarian DB - MTMT ER - TY - JOUR AU - M. Tóth, Tivadar AU - Schubert, Félix AU - Zachar, J TI - Neogene exhumation of the Variscan Szeghalom dome, Pannonian Basin, E. Hungary JF - GEOLOGICAL JOURNAL J2 - GEOL J VL - 35 PY - 2000 IS - 3-4 SP - 265 EP - 284 PG - 20 SN - 0072-1050 DO - 10.1002/gj.861 UR - https://m2.mtmt.hu/api/publication/1129800 ID - 1129800 LA - English DB - MTMT ER - TY - JOUR AU - Tari, Gábor AU - Dövényi, Péter AU - Dunkl, István AU - Horváth, Ferenc AU - Lenkey, László AU - Szafian, P AU - Toth, T TI - Lithospheric structure of the Pannonian basin derived from seismic, gravity and geothermal data JF - GEOLOGICAL SOCIETY SPECIAL PUBLICATIONS J2 - GEOL SOC SPEC PUBL VL - 156 PY - 1999 SP - 215 EP - 250 PG - 36 SN - 0305-8719 DO - 10.1144/GSL.SP.1999.156.01.12 UR - https://m2.mtmt.hu/api/publication/1256307 ID - 1256307 AB - This paper is part of the special publication No.156, The Mediterranean basins: Tertiary extension within the Alpine Orogen. (eds B.Durand, L. Jolivet, F.Horvath and M.Seranne). The structure of the Pannonian basin is the result of distinct modes of Mid-Late Miocene extension exerting a profound effect on the lithospheric configuration, which continues even today. As the first manifestation of extensional collapse, large magnitude, metamorphic core complex style extension took place at the beginning of the Mid-Miocene in certain parts of the basin. Extrapolation of the present-day high heat flow in the basin, corrected for the blanketing effect of the basin fill, indicates a hot and thin lithosphere at the onset of extension. This initial condition, combined with the relatively thick crust inherited from earlier Alpine compressional episodes, appears to be responsible for the core complex type extension at the beginning of the syn-rift period. This type of extension is well documented in the northwestern Pannonian basin. Newly obtained deep reflection seismic and fission-track data integrated with well data from the southeastern part of the basin suggests that it developed in a similar fashion. Shortly after the initial period, the style of syn-rift extension changed to a wide-rift style, covering an area of much larger geographic extent. The associated normal faults revealed by industry reflection seismic data tend to dominate within the upper crust, obscuring pre-existing structures. However, several deep seismic profiles, constrained by gravity and geothermal modeling, image the entire lithosphere beneath the basin. It is the Mid-Miocene synrift extension which is still reflected in the structure of the Pannonian lithosphere, on the scale of the whole basin system. The gradually diminishing extension during the Late Miocene/Pliocene could not advance to the localization of extension into narrow rift zones in the Pannonian region except some deep subbasins such as the Mako/Bekes and Danube basins. These basins are underlain coincidently by anomalously thin crust (22-25 km) and lithosphere (45-60 km). Significant departures (up to 130 mW m -2) from the average present-day surface heat flow for the initiation of two newly defined narrow rift zones (Tisza and Duna) in the Pannonian basin system. However, both of these narrow rifts failed since the final docking of the Eastern Carpathians onto the European foreland excluded any further extension of the back-arc region. 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 -