TY - JOUR AU - Balázs, Attila AU - Matenco, L AU - Magyar, Imre AU - Horváth, Ferenc AU - Cloetingh, S TI - The link between tectonics and sedimentation in back-arc basins: New genetic constraints from the analysis of the Pannonian Basin JF - TECTONICS J2 - TECTONICS VL - 35 PY - 2016 IS - 6 SP - 1526 EP - 1559 PG - 34 SN - 0278-7407 DO - 10.1002/2015TC004109 UR - https://m2.mtmt.hu/api/publication/3097539 ID - 3097539 N1 - Cited By :52 Export Date: 27 November 2019 Correspondence Address: Balázs, A.; Department of Geophysics and Space Science, Eötvös Loránd UniversityHungary; email: a.balazs@uu.nl Funding Agency and Grant Number: Netherlands Centre for Integrated Solid Earth Science (ISES); Eotvos Lorand University, Budapest Funding text: This study was financed by the Netherlands Centre for Integrated Solid Earth Science (ISES) and Eotvos Lorand University, Budapest, in a collaborative study of the Pannonian Basin. MOL Plc., TXM Ltd., and RAG Ltd. are acknowledged for providing seismic and well data. The first and fourth authors (A.B. and F.H.) are grateful to the academic support of the Hungarian Science Foundation (OTKA NK83400). This is MTA-MTM-ELTE Paleo contribution No. 221. Laszlo Fodor, Gabor Bada, and Endre Dombradi are thanked for the stimulating discussions about the tectonics of the area. Orsolya Sztano is thanked for insights on the sedimentological evolution of the basins. Viktor Lemberkovics is acknowledged for discussions on the Kiskunhalas subbasin. We thank Bruno Saftic and an anonymous reviewer for their detailed and constructive remarks. The data supporting this paper are available by contacting the corresponding author. AB - The architecture of sedimentary basins reflects the relationship between accommodation space and sediment supply, their rates and localization being variable during basin evolution. The mechanisms driving the interplay between tectonics and sedimentation in extensional back-arc basins overlying rheological weak zones inherited from an earlier orogenic evolution are less understood. A typical example is the Pannonian back-arc basin of Central Europe. It is floored by continental lithosphere and was affected by large amounts of extension driven by the subduction rollback that took place in the Carpathians and/or Dinarides. A novel kinematic and seismic sequence stratigraphic interpretation calibrated by wells allows the quantification of the link between the formation of half grabens and coeval sedimentation in the Great Hungarian Plain part of the basin. While the lower order tectonic-induced cycles characterize the main phases of extension in various subbasins, the higher-order cyclicity and associated unconformities define individual moments of fault (re)activation. Our novel interpretation of a temporal and spatial migration of extension during Miocene times explains the contrasting present-day strike of various subbasins as a result of their gradual clockwise rotation. Incorporating the observed asymmetry, in particular the associated footwall exhumation, infers that the amount of extension is much larger than previously thought. The quantitative link between tectonics and sedimentation has allowed the definition of a novel model of sedimentation in asymmetric basins that can be ported to other natural scenarios of similarly hyperextended back-arc basins observed elsewhere. ©2016. American Geophysical Union. All Rights Reserved. LA - English DB - MTMT ER - TY - CHAP AU - Magyar, Imre AU - Sztanó, Orsolya AU - Csillag, Gábor AU - Kercsmár, Zsolt AU - Katona, Lajos Tamás AU - Lantos, Zoltán AU - Bartha, István Róbert AU - Budai, S AU - Fodor, László ED - Šujan, Michal TI - Pannonian molluscs and their localities in the Gerecse Hills, Transdanubian Range T2 - Environmental, Structural and stratigraphical Evolution of the Western Carpathians PB - Comenius University Press CY - Bratislava SN - 9788022342025 PY - 2016 SP - 54 EP - 55 PG - 2 UR - https://m2.mtmt.hu/api/publication/3175271 ID - 3175271 LA - English DB - MTMT ER - TY - JOUR AU - Sztanó, Orsolya AU - Kováč, M AU - Magyar, Imre AU - Šujan, M AU - Fodor, László AU - Uhrin, András AU - Rybár, S AU - Csillag, Gábor AU - Tőkés, Lilla TI - Late Miocene sedimentary record of the Danube/Kisalföld Basin: interregional correlation of depositional systems, stratigraphy and structural evolution JF - GEOLOGICA CARPATHICA J2 - GEOL CARPATH VL - 67 PY - 2016 IS - 6 SP - 525 EP - 542 PG - 18 SN - 1335-0552 DO - 10.1515/geoca-2016-0033 UR - https://m2.mtmt.hu/api/publication/3159399 ID - 3159399 LA - English DB - MTMT ER - TY - CHAP AU - Bartha, István Róbert AU - Magyar, Imre AU - Fodor, László AU - Csillag, Gábor AU - Lantos, Zoltán AU - Tőkés, Lilla AU - Sztanó, Orsolya ED - Bartha, I-R ED - Kriván, Á ED - Magyar, Imre ED - Sebe, Krisztina TI - Lake Pannon Deltaic deposits in Gerecse hills, Hungary T2 - Neogene of the Paratethyan Region: 6th Workshop on the Neogene of Central and South-Eastern Europe. An RCMNS Interim Colloquium PB - Magyarhoni Földtani Társulat CY - Budapest SN - 9789638221575 PY - 2015 SP - 19 PG - 1 UR - https://m2.mtmt.hu/api/publication/2912997 ID - 2912997 LA - English DB - MTMT ER - TY - CHAP AU - Sebe, Krisztina AU - Csillag, Gábor AU - Dulai, Alfréd AU - Gasparik, Mihály AU - Magyar, Imre AU - Selmeczi, Ildikó AU - Szabó, Márton AU - Sztanó, Orsolya AU - Szuromi-Korecz, A ED - Bartha, I-R ED - Kriván, Á ED - Magyar, Imre ED - Sebe, Krisztina TI - Neogene stratigraphy in the Mecsek region. Hetvehely, Badenian rocky shore and fossiliferous shorface sand TS - Hetvehely, Badenian rocky shore and fossiliferous shorface sand T2 - Neogene of the Paratethyan Region: 6th Workshop on the Neogene of Central and South-Eastern Europe. An RCMNS Interim Colloquium PB - Magyarhoni Földtani Társulat CY - Budapest SN - 9789638221575 PY - 2015 SP - 102 EP - 124 PG - 23 UR - https://m2.mtmt.hu/api/publication/2906290 ID - 2906290 LA - English DB - MTMT ER - TY - JOUR AU - Sztanó, Orsolya AU - Sebe, Krisztina AU - Csillag, Gábor AU - Magyar, Imre TI - Erratum: Turbidites as indicators of paleotopography, Upper Miocene Lake Pannon, Western Mecsek Mountains (Hungary) (Geologica Carpathica (2015) 66: 4 (331-344) DOI: 10.1515/geoca-2015-0029) JF - GEOLOGICA CARPATHICA J2 - GEOL CARPATH VL - 66 PY - 2015 IS - 5 SP - 439 EP - 439 PG - 1 SN - 1335-0552 DO - 10.1515/geoca-2015-0036 UR - https://m2.mtmt.hu/api/publication/3114745 ID - 3114745 N1 - WoS:hiba:000364857800007 2020-08-29 19:08 cím nem egyezik LA - English DB - MTMT ER - TY - JOUR AU - Sztanó, Orsolya AU - Sebe, Krisztina AU - Csillag, Gábor AU - Magyar, Imre TI - Turbidites as indicators of paleotopography, Upper Miocene Lake Pannon, Western Mecsek Mountains (Hungary) JF - GEOLOGICA CARPATHICA J2 - GEOL CARPATH VL - 66 PY - 2015 IS - 4 SP - 331 EP - 344 PG - 14 SN - 1335-0552 DO - 10.1515/geoca-2015-0029 UR - https://m2.mtmt.hu/api/publication/2934948 ID - 2934948 N1 - Eötvös Loránd University, Department of Physical and Applied Geology, Pazmany Peter setany 1/c, Budapest, 1117, Hungary University of Pécs, Department of Geology and Meteorology, Ifjúság ut. 6, Pécs, 7624, Hungary Geological and Geophysical Institute of Hungary, Stefánia ut. 14, Budapest, 1143, Hungary MOL Hungarian Oil and Gas Plc., Október huszonharmadika ut. 18, Budapest, 1117, Hungary MTA-MTM-ELTE Research Group for Paleontology, P.O. Box 137, Budapest, 1431, Hungary Cited By :12 Export Date: 13 July 2022 LA - English DB - MTMT ER - TY - JOUR AU - Magyar, Imre AU - Radivojević, D AU - Sztanó, Orsolya AU - Synak, R AU - Ujszászi, K AU - Pócsik, M TI - Progradation of the paleo-Danube shelf margin across the Pannonian Basin during the Late Miocene and Early Pliocene JF - GLOBAL AND PLANETARY CHANGE J2 - GLOBAL PLANET CHANGE VL - 103 PY - 2013 IS - 1 SP - 168 EP - 173 PG - 6 SN - 0921-8181 DO - 10.1016/j.gloplacha.2012.06.007 UR - https://m2.mtmt.hu/api/publication/2154674 ID - 2154674 N1 - MOL Hungarian Oil and Gas Plc., Október 23. u. 18., H-1117 Budapest, Hungary Research Group for Paleontology, Hungarian Academy of Sciences, Hungarian Natural History Museum-Eötvös University, POB 137, H-1431 Budapest, Hungary NIS Gazprom Neft, Narodnog fronta 12, 21000 Novi Sad, Serbia Eötvös Loránd University, Pázmány Péter sétany 1/c, H-1117 Budapest, Hungary Comenius University, Mlynská dolina, 84215 Bratislava, Slovakia Cited By :100 Export Date: 27 November 2019 CODEN: GPCHE Correspondence Address: Magyar, I.; MOL Hungarian Oil and Gas Plc., Október 23. u. 18., H-1117 Budapest, Hungary; email: immagyar@mol.hu AB - The basin of giant Lake Pannon in Central Europe was filled by forward accretion of sediment packages during the Late Miocene and Early Pliocene. Successive positions of the shelf-margin are represented by a series of clinoforms in seismic profiles. The height of the clinoforms (and thus the inferred paleo water depth) is 200-600 m in the successions; the width of the slope, measured from the shelf-break down to the toe of slope, varies between 5 and 15 km. Geographical position of successive shelf-margin slopes indicates that about 2/3 of the basin area was filled by sediment transport systems supplying sediments from the NW, from the Alps and Western Carpathians. The first shelf-margin slope was built by the paleo-Danube in the Kisalföld/Danube sub-basin about 10 Ma ago, and during the subsequent 6 Ma it prograded ca. 400 km to the SE across the Pannonian Basin, with an average of 67 km/Ma slope advance. The most significant agent of this shelf growth was the sediment dispersal system of the paleo-Danube, hence we designate this northwestern shelf the paleo-Danube shelf. The northeastern part of Lake Pannon was filled by the paleo-Tisza system, supplying sediments from the Northeastern and Eastern Carpathians. Additional local systems carried sediments from E to W along the eastern margin and S to N along the southern margin of the Pannonian Basin, respectively. The deep-water environment disappeared from the Pannonian Basin and the endemic, brackish biota of Lake Pannon went extinct probably 4 Ma ago, when the paleo-Danube shelf margin and a (yet unidentified) shelf margin prograding in the opposite direction met in the southeastern corner of the Pannonian Basin. © 2012 Elsevier B.V. All rights reserved. LA - English DB - MTMT ER - TY - JOUR AU - Sztanó, Orsolya AU - Magyar, Imre AU - Szónoky, Miklós AU - Lantos, Miklós AU - Müller, Pál AU - Lenkey, László AU - Katona, Lajos Tamás AU - Csillag, Gábor TI - A Tihanyi Formáció a Balaton környékén: típusszelvény, képződési körülmények, rétegtani jellemzés. Tihany Formation in the surroundings of Lake Balaton: Type locality, depositional setting and stratigraphy TS - Tihany Formation in the surroundings of Lake Balaton: Type locality, depositional setting and stratigraphy JF - FÖLDTANI KÖZLÖNY J2 - FÖLDTANI KÖZLÖNY VL - 143 PY - 2013 IS - 1 SP - 73 EP - 98 PG - 26 SN - 0015-542X UR - https://m2.mtmt.hu/api/publication/2498680 ID - 2498680 N1 - ELTE Általános és Alkalmazott Földtani Tanszék, Pázmány sétány 1/C, 1117 Budapest, Hungary MTA-MTM-ELTE Paleontológiai Kutatócsoport, Pf. 137, 1431 Budapest, Hungary Szegedi Tudományegyetem, Föld- és Oslénytani Tanszék, Egyetem u. 2-6, 6722 Szeged, Hungary Magyar Földtani és Geofizikai Intézet, Stefánia út 14, 1143 Budapest, Hungary MTA-ELTE Geológiai, Geofizikai és Urtudományi Kutatócsoport, Pázmány sétány 1/C, 1117 Budapest, Hungary Bakonyi Természettudományi Múzeum, Rákóczi tér 3-5, 8420 Zirc, Hungary Cited By :16 Export Date: 27 November 2019 Correspondence Address: Sztanó, O.; ELTE Általános és Alkalmazott Földtani Tanszék, Pázmány sétány 1/C, 1117 Budapest, Hungary; email: sztano@caesar.elte.hu AB - MatarkaID=1911933 LA - English DB - MTMT ER - TY - CHAP AU - Magyar, Imre AU - Geary, DH ED - Baganz, OW ED - Bartov, Y ED - Bohacs, K ED - Nummedal, D TI - Biostratigraphy in a late Neogene Caspian-Type Lacustrine Basin: Lake Pannon, Hungary T2 - Lacustrine sandstone reservoirs and hydrocarbon systems PB - American Association of Petroleum Geologists (AAPG) CY - Tulsa (OK) SN - 9780891813774 T3 - AAPG Memoir, ISSN 0271-8529 ; 95. PY - 2012 SP - 255 EP - 264 PG - 10 DO - 10.1306/13291392M953142 UR - https://m2.mtmt.hu/api/publication/2145538 ID - 2145538 N1 - Cited By :33 Export Date: 15 February 2022 LA - English DB - MTMT ER - TY - JOUR AU - Konrád, Gyula AU - Sebe, Krisztina TI - Fiatal tektonikai jelenségek új észlelései a Nyugati-Mecsekben és környezetében JF - FÖLDTANI KÖZLÖNY J2 - FÖLDTANI KÖZLÖNY VL - 140 PY - 2010 IS - 2 SP - 135 EP - 161 PG - 24 SN - 0015-542X UR - https://m2.mtmt.hu/api/publication/1354802 ID - 1354802 N1 - 160.o. bibl. AB - Exposures of Neogene and Quaternary age were investigated along the main structural zones of the Western Mecsek Mts. (SW Hungary) in order to study post-Miocene tectonic activity, with an aim of supplementing studies on the longterm stability of the region. Field observations showed that young movements affected only the mountain fronts and the foreland. From the 24 studied exposures, those with impacts of tectonic activity were located along the major fault zones of the Western Mecsek Mts. and prove tectonic/seismic events occurring as late as the Late Pleistocene along the Mecsekalja Dislocation Zone and probably the Hetvehely–Magyarszék Fault. On the contrary, no impact of neotectonic activity was found within the Western Mecsek Anticline, indicating that this area behaved as a single solid block during post-Miocene movements. Since the Karpatian age, 5 tectonic phases could be distinguished. From these – somewhat opposing previous research – transtension seems typical for the Karpatian along the Hetvehely–Magyarszék Fault. The Early Pannonian transtensional stress field did not cease to exist at the beginning of the Late Pannonian. Tectonic inversion started only within the first half of the Late Pannonian and can be considered active up to present day in the major part of the area. A munka során a Nyugat-Mecsek fő szerkezeti vonalainak környezetében feltárt neogén és kvarter képződményeket vizsgáltuk fiatal (posztpannóniai) tektonikai aktivitás nyomai után kutatva, elsősorban a terület hosszú távú stabilitásának megítéléséhez. A terepi megfigyelések alapján a fiatal mozgások csak a hegységperemet és az előteret érintették. A vizsgált 24 feltárásból a fiatal tektonikával érintettek a Nyugat-Mecsek meghatározó szerkezeti vonalai mentén helyezkednek el, és még a késő-pleisztocénben is szerkezeti mozgásokat, illetve szeizmikus aktivitást bizonyítanak a Mecsekalja-öv és valószínűleg a Hetvehely–magyarszéki-törés mentén. Ezzel ellentétben a Nyugatmecseki- antiklinális területén belül neotektonikára utaló jeleket nem észleltünk, ez alapján a pannóniai–negyedidőszaki mozgások során a Nyugat-Mecsek egységes tömbként viselkedhetett. A kárpáti korszak óta öt tektonikai fázis volt elkülöníthető a területen. Ezek közül – a korábbi vizsgálati eredményekkel szemben – a kárpáti korszakra jellemzőnek tűnik a transztenzió a Hetvehely–magyarszéki-törés mentén. A kora-pannóniai transztenziós feszültségtér a Mecsekalja-öv mentén még a késő-pannóniai elején is fennállt. Az inverzió a késő-pannóniai első felében kezdődött és a terület legnagyobb részén máig aktívnak tekinthető. LA - Hungarian DB - MTMT ER - TY - JOUR AU - Cziczer, István AU - Magyar, Imre AU - Pipik, R AU - Bohme, M AU - Coric, S AU - Bakrac, K AU - Suto-Szentai, M AU - Lantos, M AU - Babinszki, Edit AU - Muller, P TI - Life in the sublittoral zone of long-lived Lake Pannon: paleontological analysis of the Upper Miocene Szak Formation, Hungary. Paleontological analysis of the Upper Miocene Szák Formation, Hungary TS - Paleontological analysis of the Upper Miocene Szák Formation, Hungary JF - INTERNATIONAL JOURNAL OF EARTH SCIENCES J2 - INT J EARTH SCI VL - 98 PY - 2009 IS - 7 SP - 1741 EP - 1766 PG - 26 SN - 1437-3254 DO - 10.1007/s00531-008-0322-3 UR - https://m2.mtmt.hu/api/publication/1333817 ID - 1333817 N1 - Department of Geology and Paleontology, University of Szeged, Egyetem u. 2-6, 6722 Szeged, Hungary MOL Hungarian Oil and Gas Plc, Október 23. u. 18, 1117 Budapest, Hungary Slovak Academy of Sciences, Geological Institute, Severná 5, 974 01 Banská Bystrica, Slovakia Department on Earth- and Environmental Science, Section Palaeontology, Ludwig-Maximilians University, Munich Richard-Wagner-Str. 10, 80333 Munich, Germany Geological Survey of Austria, Neulinggasse 38, 1030 Vienna, Austria Croatian Geological Survey, Sachsova 2, 10000 Zagreb, Croatia Május 1. u. 7, 7300 Komlo', Hungary Geological Institute of Hungary, Stefánia út 14, 1143 Budapest, Hungary Cited By :55 Export Date: 31 August 2023 CODEN: IJESF Correspondence Address: Cziczer, L.; Department of Geology and Paleontology, Egyetem u. 2-6, 6722 Szeged, Hungary; email: cziczer@yahoo.com AB - Life and depositional environments in the sublittoral zone of Lake Pannon, a large, brackish Paratethyan lake from the Late Miocene, were reconstructed from fossils and facies of the Szak Formation. This formation is exposed in several, roughly coeval (9.4-8.9 Ma) outcrops, located along strike of the paleo-shelf-break in northwestern Hungary. The silty argillaceous marl of the formation was deposited below storm wave base, at 20-30 to 80-90 m water depth. The abundance of benthic organisms indicates that the bottom water was usually well oxygenated. Interstitial dysoxia, however, may have occurred immediately below the sediment-water interface, as evidenced by occasional preservation of trace fossils such as Diplocraterion. The fauna comprised endemic mollusks, including brackish cockles of the subfamily Lymnocardiinae, dreissenid mussels (Congeria), and highly adapted, uniquely large-sized deep-water pulmonate snails (planorbids and lymnaeids). Ostracods were dominated by endemic species and, in some cases, endemic genera of candonids, leptocytherids, cypridids, and loxoconchids. Fish remnants include a sciaenid otolith and the oldest skeletal occurrence of Perca in Europe. The phytoplankton comprised exclusively endemic coccolithophorids, mostly endemic dinoflagellates (prevailingly Spiniferites), and cosmopolitan green algae. The Late Miocene fauna and flora of Lake Pannon were in many ways similar to the modern Caspian biota, and in particular cases can be regarded as its precursor. LA - English DB - MTMT ER - TY - JOUR AU - Kocsis, László AU - Vennemann, TW AU - Hegner, E AU - Fontignie, D AU - Tütken, T TI - Constraints on Miocene oceanography and climate in the Western and Central Paratethys: O-, Sr-, and Nd-isotope compositions of marine fish and mammal remains JF - PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY J2 - PALAEOGEOGR PALAEOCL VL - 271 PY - 2009 IS - 1-2 SP - 117 EP - 129 PG - 13 SN - 0031-0182 DO - 10.1016/j.palaeo.2008.10.003 UR - https://m2.mtmt.hu/api/publication/3189094 ID - 3189094 AB - The Paratethys evolved as a marginal sea during the Alpine-Himalayan orogeny in the Oligo-Miocene. Sediments from the northern Alpine Molasse Basin, the Vienna, and the Pannonian Basins located in the western and central part of the Paratethys thus provide unique information on regional changes in climate and oceanography during a period of active Alpine uplift. Oxygen isotope compositions of well-preserved phosphatic fossils recovered from the sediments support deposition under sub-tropical to warm-temperate climate with water temperatures of 14 to 28 °C for the Miocene. δ18O values of fossil shark teeth are similar to those reported for other Miocene marine sections and, using the best available estimates of their biostratigraphic age, show a variation until the end of the Badenian similar to that reported for composite global record. The 87Sr/86Sr isotope ratios of the fossils follow the global Miocene seawater trend, albeit with a much larger scatter. The deviations of 87Sr/86Sr in the samples from the well-constrained seawater curve are interpreted as due to local input of terrestrially-derived Sr. Contribution of local sources is also reflected in the εNd values, consistent with input from ancient crystalline rocks (e.g., Bohemian Massif) and/or Mesozoic sediments with εNd < - 9. On the other hand, there is evidence for input from areas with Neogene volcanism as suggested by samples with elevated εNd values > - 7. Excluding samples showing local influence on the water column, an average εNd value of - 7.9 ± 0.5 may be inferred for the Miocene Paratethys. This value is indistinguishable from the εNd value of the contemporaneous Indian Ocean, supporting a dominant role of this ocean in the Western and Central Paratethys. © 2008 Elsevier B.V. All rights reserved. LA - English DB - MTMT ER - TY - JOUR AU - Csontos, László AU - Benkovics, L AU - Bergerat, F AU - Mansy, JL AU - Worum, G TI - Tertiary deformation history from seismic section study and fault analysis in a former European Tethyan margin (the Mecsek-Villany area, SW Hungary) JF - TECTONOPHYSICS J2 - TECTONOPHYSICS VL - 357 PY - 2002 IS - 1-4 SP - 81 EP - 102 PG - 22 SN - 0040-1951 DO - 10.1016/S0040-1951(02)00363-3 UR - https://m2.mtmt.hu/api/publication/2899890 ID - 2899890 N1 - Cited By :51 Export Date: 20 January 2023 Correspondence Address: Csontos, L.; Geological Department, Pazmany Péter setany l/c, Budapest 1117, Hungary; email: hungary.laszlo.csontos@ludens.elte.hu AB - Outcrop-scale structural data and seismic section interpretation are combined to unveil a very complicated Tertiary deformation history of a once Tethyan margin: the Mecsek-Villany area of Hungary. This combination of data helped to reconstruct the possible activity of individual fault zones. At least four ENE-WSW striking zones-the Northern Imbricates, the South Mecsek zone, the Gorcsony-Mariakemend ridge and the Villany Mountains-were confirmed as regional long-lived transpressive zones with very complicated internal deformation, frequently with oppositely dipping thrust faults. Tertiary structural history began with a roughly N-S-directed shortening in the South Mecsek zone. It was followed by a NE-SW-directed transpression activating practically all important wrench zones together with perpendicular transfer faults. Basins were created along some of these deformation zones, but were also affected by major tilts due to inversion. After a relatively quiescent period in the Middle Miocene, the Late Sarmatian inversion followed. Shortly after, this event was relayed by a NE-SW-directed extension-transtension. An important inversion period characterised by NW-SE compression occurred in Late Pannonian (Messinian), when all the former wrench zones were reactivated as right-lateral shear. This event is responsible for the present topography of the region. (C) 2002 Elsevier Science B.V. All rights reserved. LA - English DB - MTMT ER - TY - CHAP AU - Fodor, László AU - Csontos, L AU - Bada, G AU - Györfi, I AU - Benkovics, L ED - Durand, B ED - Jolivet, L ED - Horváth, Ferenc ED - Seranne, M TI - Tertiary tectonic evolution of the Pannonian Basin system and neighbouring orogens: a new synthesis of palaeostress data T2 - The Mediterranean Basins: tertiary extension within the Alpine Orogen PB - Geological Society of London CY - London SN - 9781862390331 T3 - Geological Society Special Publication, ISSN 0305-8719 ; 156. PY - 1999 SP - 295 EP - 334 PG - 40 DO - 10.1144/GSL.SP.1999.156.01.15 UR - https://m2.mtmt.hu/api/publication/1369059 ID - 1369059 N1 - Dept. of Appl. and Environ. Geology, Eötvös University, 1088 Múzeum krt 4/a, Budapest, Hungary Dept. of Gen. and Historical Geology, Eötvös University, 1088 Múzeum krt 4/a, Budapest, Hungary Department of Geophysics, Eötvös University, 1085 Ludovika tér 2, Budapest, Hungary Department of Engineering Geology, Technical University of Budapest, Stoczek u. 2, Budapest, Hungary Cited By :375 Export Date: 10 May 2023 Correspondence Address: Fodor, L.; Dept. of App. + Envtml. Geol., Muzeum krt 4/a, Budapest 1088, Hungary LA - English DB - MTMT ER - TY - JOUR AU - Horváth, Ferenc AU - Tari, Gábor TI - IBS Pannonian Basin project: a review of the main results and their bearings on hydrocarbon exploration JF - GEOLOGICAL SOCIETY SPECIAL PUBLICATIONS J2 - GEOL SOC SPEC PUBL VL - 156 PY - 1999 IS - 1 SP - 195 EP - 213 PG - 19 SN - 0305-8719 DO - 10.1144/GSL.SP.1999.156.01.11 UR - https://m2.mtmt.hu/api/publication/2176407 ID - 2176407 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 IBS Pannonian Basin project presents a good example of fruitful joint activity between Hungarian and other European scientists, and beneficial co-operation of academia and the petroleum industry. This allowed us to achieve significant progress in the understanding of the structure, tectonic evolution, stratigraphic features and hydrocarbon generation in the Pannonian Basin. The Pannonian region has been an integral part of the Alpine belt, and it reveals the complexity of orogenic evolution. Continental to oceanic rifting, followed by convergence, subduction and continental collision shaped the Palaeozoic-Mesozoic substrata of the region. Subsequently, two periods of basin formation (Late Cretaceous and Palaeogene) occurred, most probably in compressional setting. From the earliest Miocene large scale lateral displacement and block rotation took place in the internal domain of the orogen, together with the formation of the Pannonian Basin. This has been characterized by lithospheric extension, however, interrupted by compressional events. The modern Pannonian Basin is in an initial phase of positive structural inversion. All of these tectonic events had significant impacts on the formation and the economic value of the various petroleum systems in the area. LA - English DB - MTMT ER - TY - JOUR AU - Magyar, Imre AU - Geary, DH AU - Muller, P TI - Paleogeographic evolution of the Late Miocene Lake Pannon in Central Europe JF - PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY J2 - PALAEOGEOGR PALAEOCL VL - 147 PY - 1999 IS - 3-4 SP - 151 EP - 167 PG - 17 SN - 0031-0182 DO - 10.1016/S0031-0182(98)00155-2 UR - https://m2.mtmt.hu/api/publication/1890263 ID - 1890263 N1 - Cited By :351 Export Date: 24 February 2023 CODEN: PPPYA Correspondence Address: Geary, D.H.; Department of Geology and Geophysics, 1215 West Dayton Street, Madison, WI 53706, United States; email: dana@geology.wisc.edu AB - The paleogeographic evolution of Lake Pannon within the Pannonian basin is reconstructed with eight maps, ranging from the Middle Miocene to the Early Pliocene. The maps are based on the distribution of selected biozones and specific fossils, and on complementary sedimentological and seismic information. Our reconstruction shows that the history of Lake Pannon can be divided into three distinct intervals: an initial stage with low water level, which resulted in isolation from the sea at about 12 Ma and might have led to temporary fragmentation of the lake; an interval of gradual transgression lasting until ca. 9.5 Ma; and a long late interval of shrinkage and infilling of sediments that persisted into the Early Pliocene. The deep subbasins of the lake formed during the transgressive interval, in more basinward locations than the deep basins of the preceding Sarmatian age. The southern shoreline, running parallel with the Sava and Danube rivers along the northern foot of the Dinarides, changed very Little during the Lifetime of the lake, while the northern shoreline underwent profound changes. (C) 1999 Elsevier Science B.V. All rights reserved. LA - English DB - MTMT ER - TY - JOUR AU - Horváth, Ferenc AU - Cloetingh, S TI - Stress-induced late-stage subsidence anomalies in the Pannonian basin JF - TECTONOPHYSICS J2 - TECTONOPHYSICS VL - 266 PY - 1996 IS - 1-4 SP - 287 EP - 300 PG - 14 SN - 0040-1951 DO - 10.1016/S0040-1951(96)00194-1 UR - https://m2.mtmt.hu/api/publication/1255454 ID - 1255454 N1 - DE: basin evolution; basin modeling; tectonic inversion; intraplate stress AB - Subsidence, sedimentation and tectonic quiescence of the Pannonian basin was interrupted a few million years ago by tectonic reactivation. This recent activity has manifested itself in uplift of the western and eastern flanks, and continuing subsidence of the central part of the Pannonian basin. Low- to medium-magnitude earthquakes of the Carpathian-Pannonian region are generated mostly in the upper crust by reverse and wrench fault mechanisms. There is no evidence for earthquakes of extensional origin. 2-D model calculation of the subsidence history shows that a recent increase in magnitude of horizontal compressional intraplate stress can explain fairly well the observed Quaternary uplift and subsidence pattern. We propose that this stress increase is caused by the overall Europe/Africa convergence. In Late Pliocene, consumption of subductible lithosphere at the eastern margin of the Pannonian basin was completed, and the lithosphere underlying the Pannonian basin became locked in a stable continental frame. Consequently extensional basin formation has come to an end, and compressional inversion of the Pannonian basin is in progress. 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 -