TY - JOUR AU - Molnár, László AU - M. Tóth, Tivadar AU - Schubert, Félix TI - Statistical characterization of brittle and semi-brittle fault rocks: a clast geometry approach JF - ACTA GEODAETICA ET GEOPHYSICA J2 - ACTA GEOD GEOPHYS VL - 49 PY - 2014 IS - 4 SP - 527 EP - 550 PG - 24 SN - 2213-5812 DO - 10.1007/s40328-014-0067-3 UR - https://m2.mtmt.hu/api/publication/2783510 ID - 2783510 N1 - Funding Agency and Grant Number: MOL Hungarian Oil and Gas Company Funding text: We thank MOL Hungarian Oil and Gas Company for providing the samples and the financial support of this research. We are grateful to Gyula Maros (Hungarian Geological and Geophysical Institute) for his help in the use of ImaGeo corescanner. English was corrected by Proof-Reading-Service.com. Cited By :2 Export Date: 12 February 2021 Correspondence Address: Molnár, L.; Department of Mineralogy, Egyetem utca 2, Hungary Funding text 1: Acknowledgments We thank MOL Hungarian Oil and Gas Company for providing the samples and the financial support of this research. We are grateful to Gyula Maros (Hungarian Geological and Geophysical Institute) for his help in the use of ImaGeo corescanner. English was corrected by Proof-Reading-Service.com. Cited By :2 Export Date: 12 September 2021 Correspondence Address: Molnár, L.; Department of Mineralogy, Egyetem utca 2, Hungary Funding text 1: Acknowledgments We thank MOL Hungarian Oil and Gas Company for providing the samples and the financial support of this research. We are grateful to Gyula Maros (Hungarian Geological and Geophysical Institute) for his help in the use of ImaGeo corescanner. English was corrected by Proof-Reading-Service.com. LA - English DB - MTMT ER - TY - CHAP AU - Vass, I AU - M. Tóth, Tivadar AU - Szanyi, János AU - Kovács, Balázs ED - M. Tóth, Tivadar TI - Az aljzati kristályos hátak szerepe az Alföld fluidum áramlási és hőtranszport folyamataiban 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 - 325 EP - 339 PG - 15 UR - https://m2.mtmt.hu/api/publication/1382869 ID - 1382869 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 - Horváth, Ferenc AU - Bada, G AU - Szafián, P AU - Tari, Gábor AU - Ádám, A AU - Cloetingh, S TI - Formation and deformation of the Pannonian Basin: Constraints from observational data JF - MEMOIRS OF THE GEOLOGICAL SOCIETY OF LONDON J2 - MEM GEOL SOC LOND VL - 32 PY - 2006 SP - 191 EP - 206 PG - 16 SN - 9781862392120 SN - 0435-4052 DO - 10.1144/GSL.MEM.2006.032.01.11 UR - https://m2.mtmt.hu/api/publication/2176402 ID - 2176402 N1 - Megjegyzés-22854802 BE Stephenson, RA AB - The past decade has witnessed spectacular progress in the collection of observational data and their interpretation in the Pannonian Basin and the surrounding Alpine, Carpathian and Dinaric mountain belts. A major driving force behind this progress was the PANCARDI project of the EUROPROBE programme. The paper reviews tectonic processes, structural styles, stratigraphic records and geochemical data for volcanic rocks. Structural and seismic sections of different scales, seismic tomography and magnetotelluric, gravity and geothermal data are also used to determine the deformational styles, and to compile new crustal and lithospheric thickness maps of the Pannonian Basin and the surrounding fold-and-thrust belts. The Pannonian Basin is superimposed on former Alpine terranes. Its formation is a result of extensional collapse of the overthickened Alpine orogenic wedge during orogen-parallel extrusion towards a 'free boundary' offered by the roll-back of the subducting Carpathian slab, As a conclusion, continental collision and back-arc basin evolution is discussed as a single, complex dynamic process, with minimization of the potential and deformational energy as the driving principle. © The Geological Society of London 2006. LA - English DB - MTMT ER - TY - JOUR AU - M. Tóth, Tivadar AU - Szűcs, É AU - Schubert, Félix AU - Hollós, Cs TI - Conceptual fracture network model of the crystalline basement of the Szeghalom Dome (Pannonian Basin, SE Hungary) JF - ACTA GEOLOGICA HUNGARICA: A QUARTERLY OF THE HUNGARIAN ACADEMY OF SCIENCES J2 - ACTA GEOL HUNG VL - 47 PY - 2004 IS - 1 SP - 19 EP - 34 PG - 16 SN - 0236-5278 DO - 10.1556/AGeol.47.2004.1.2 UR - https://m2.mtmt.hu/api/publication/1129815 ID - 1129815 LA - English DB - MTMT ER - TY - JOUR AU - Juhász, A AU - M. Tóth, Tivadar AU - Ramseyer, K AU - Matter, A TI - Connected fluid evolution in fractured crystalline basement and overlying sediments, Pannonian Basin, SE Hungary JF - CHEMICAL GEOLOGY J2 - CHEM GEOL VL - 182 PY - 2002 IS - 2-4 SP - 91 EP - 120 PG - 30 SN - 0009-2541 DO - 10.1016/S0009-2541(01)00269-8 UR - https://m2.mtmt.hu/api/publication/1129807 ID - 1129807 LA - English DB - MTMT ER - TY - JOUR AU - Kovács, Sándor AU - Szederkényi, T AU - Haas, János AU - Buda, György AU - Császár, Géza AU - Nagymarosy, András TI - Tectonostratigraphic terranes in the pre-Neogene basement of the Hungarian part of the Pannonian area JF - ACTA GEOLOGICA HUNGARICA: A QUARTERLY OF THE HUNGARIAN ACADEMY OF SCIENCES J2 - ACTA GEOL HUNG VL - 43 PY - 2000 IS - 3 SP - 225 EP - 328 PG - 104 SN - 0236-5278 UR - https://m2.mtmt.hu/api/publication/152233 ID - 152233 N1 - Cited By :96 Export Date: 13 January 2023 Correspondence Address: Kovávs, S.; Geological Research Group, Muzeum krt. 4/a, Budapest, Buda H-1088, Hungary 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 - Csontos, L AU - Nagymarosy, András TI - The mid-Hungarian line: a zone of repeated tectonic inversions JF - TECTONOPHYSICS J2 - TECTONOPHYSICS VL - 297 PY - 1998 IS - 1-4 SP - 51 EP - 71 PG - 21 SN - 0040-1951 DO - 10.1016/S0040-1951(98)00163-2 UR - https://m2.mtmt.hu/api/publication/2899915 ID - 2899915 N1 - Hiányzó város: 'LINDABRUNN' Megjegyzés-22049443 Z9: 75 WC: Geochemistry & Geophysics AB - The Mid-Hungarian line is a major tectonic feature of the Intra-Carpathian area separating two terranes of different origin and tectonic structure. Although this tectonic line was known from borehole records, it has not been described in seismic sections. The study presents interpreted seismic lines crossing the supposed trace of the Mid-Hungarian line. These seismic sections show north-dipping normal faults and thrust faults as well as cross-cutting young strike-slip faults. A complex tectonic history is deduced, including intra-Oligocene-Early Miocene thrusting, Middle Miocene extension, local Late Miocene inversion and Late Miocene-Pliocene normal faulting and left-lateral wrenching. In the light of our seismic study we think that the best candidate for the Mid-Hungarian line is a north-dipping detachment fault beneath large masses of Neogene volcanics. The auxiliary structures to the north seen on seismic sections suggest that it moved as a south-vergent thrust fault during the Palaeogene-Early Miocene which later was reactivated as a set of normal faults. The northern Alcapa unit overrode the southern Tisza-Dacia unit along this fault zone. The same relative positions are observed in the northern termination of the line. Other structures along the supposed trace of the line are north-dipping normal-or strike-slip faults which frequently were reactivated as smaller thrust faults during the late Neogene. Palaeogene-Early Miocene thrusting along the line might be the result of the opposite Tertiary rotations of the two major units, as suggested by palaeomagnetic measurements and earlier models. (C) 1998 Elsevier Science B.V. All rights reserved. LA - English DB - MTMT ER - TY - JOUR AU - Posgay, Károly AU - Bodoky, Tamás János AU - Hegedűs, Endre AU - Kovácsvölgyi, S AU - Lenkey, László AU - Szafián, P AU - Takács, Ernő AU - Csabafi, Róbert Imre AU - Varga, G TI - Asthenospheric structure beneath a Neogene basin in southeast Hungary JF - TECTONOPHYSICS J2 - TECTONOPHYSICS VL - 252 PY - 1995 IS - 1-4 SP - 467 EP - 484 PG - 18 SN - 0040-1951 DO - 10.1016/0040-1951(95)00098-4 UR - https://m2.mtmt.hu/api/publication/1441803 ID - 1441803 N1 - Eötvös Loránd Geophysical Institute of Hungary, Columbus u. 17-23, H-1145 Budapest, Hungary Eötvös Loránd University H-1083 Budapest, Ludovika tér, Hungary Cited By :95 Export Date: 19 December 2022 Correspondence Address: Posgay, K.; Eötvös Loránd Geophysical Institute of Hungary, Columbus u. 17-23, H-1145 Budapest, Hungary 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 -