TY - CHAP AU - Less, György AU - Grill, J AU - Szentpétery, I AU - Róth, L AU - Gyuricza, György ED - Szentpétery, I ED - Less, György TI - Az Aggtelek-Rudabányai-hegység fedetlen földtani térképe M=1:25 000, 1988 (ISBN: 963 671 119 4 CI) T2 - Az Aggtelek–Rudabányai-hegység földtana PB - Magyar Állami Földtani Intézet (MÁFI) CY - Budapest SN - 9636712557 PY - 2006 SP - 1 A/0 EP - 2 A/0 UR - https://m2.mtmt.hu/api/publication/2145815 ID - 2145815 LA - Hungarian DB - MTMT ER - TY - JOUR AU - Péró, Csaba AU - Kovács, Sándor AU - Less, György AU - Fodor, László TI - Geological setting of Triassic "Hallstatt" (s.l.) facies in NE Hungary JF - ANNALES UNIVERSITATIS SCIENTIARUM BUDAPESTINENSIS DE ROLANDO EÖTVÖS NOMINATAE - SECTIO GEOLOGICA J2 - ANN UNIV SCI BP R EÖTVÖS NOM SECT GEOL VL - 35 PY - 2003 SP - 58 EP - 60 PG - 3 SN - 0365-0634 UR - https://m2.mtmt.hu/api/publication/152210 ID - 152210 LA - English DB - MTMT ER - TY - JOUR AU - Csontos, L AU - Márton Péterné Szalay, Emőke AU - Wórum, G AU - Benkovics, L TI - Geodynamics of SW-Pannonian inselbergs (Mecsek and Villány Mts, SW Hungary): inferences from a complex structural analysis JF - EGU STEPHAN MUELLER SPECIAL PUBLICATION SERIES J2 - EGU STEPHAN MUELLER SPEC PUBL SER VL - 3 PY - 2002 SP - 1 EP - 19 PG - 19 SN - 1868-4556 UR - https://m2.mtmt.hu/api/publication/1155431 ID - 1155431 LA - English DB - MTMT ER - TY - JOUR AU - Fodor, László AU - Jelen, B AU - Márton Péterné Szalay, Emőke AU - Zupancic, N AU - Trajanova, M AU - Rifelj, H AU - Pécskay, Zoltán AU - Balogh, Kadosa AU - Koroknai, B AU - Dunkl, István AU - Horváth, Péter AU - Horvat, A AU - Vrabec, M AU - Kraljic, M AU - Kevric, R TI - Connection of neogene basin formation, magmatism and cooling of metamorphics in NE Slovenia. JF - GEOLOGICA CARPATHICA J2 - GEOL CARPATH VL - 53 PY - 2002 IS - Special Issue SP - 199 EP - 201 PG - 3 SN - 1335-0552 UR - https://m2.mtmt.hu/api/publication/1621179 ID - 1621179 N1 - [ATKI P15669] LA - English DB - MTMT ER - TY - JOUR AU - Márton Péterné Szalay, Emőke AU - Pavelić, D AU - Tomljenović, B AU - Avanić, R AU - Pamić, J AU - Márton, Péter TI - In the wake of a countercklockwise rotating Adriatic microplate: Neogene paleomagnetic results from northern Croatia JF - INTERNATIONAL JOURNAL OF EARTH SCIENCES J2 - INT J EARTH SCI VL - 91 PY - 2002 SP - 514 EP - 523 PG - 10 SN - 1437-3254 DO - 10.1007/s00531-001-0249-4 UR - https://m2.mtmt.hu/api/publication/1042243 ID - 1042243 N1 - Eötvös Loránd Geophysical Institute of Hungary, Paleomagnetic Laboratory, 1145 Budapest, Columbus 17-23, Hungary Institute of Geology, Sachsova 2, 10000 Zagreb, Croatia University of Zagreb, Faculty of Mining, Geology and Petroleum Engineering, Pierottijeva 6, 10000 Zagreb, Croatia Croatian Academy of Sciences and Arts, A. Kovacica 5, 10000 Zagreb, Croatia Eötvös Loránd University, Geophysics Department, Ludovika tér 2, 1082 Budapest, Hungary Cited By :55 Export Date: 12 January 2024 CODEN: IJESF Correspondence Address: Márton, E.; Eotvos Lorand Geophysical Inst. Hung, Columbus 17-23, Budapest 1145, Hungary; email: paleo@elgi.hu LA - English DB - MTMT ER - TY - JOUR AU - Tomljenovic, B AU - Csontos, László TI - Neogene-quaternary structures in the border zone between Alps, Dinarides and Pannonian Basin (Hrvatsko zagorje and Karlovac Basins, Croatia) JF - INTERNATIONAL JOURNAL OF EARTH SCIENCES J2 - INT J EARTH SCI VL - 90 PY - 2001 IS - 3 SP - 560 EP - 578 PG - 19 SN - 1437-3254 DO - 10.1007/s005310000176 UR - https://m2.mtmt.hu/api/publication/2899897 ID - 2899897 N1 - Hiányzó város: 'TUBINGEN' AB - Analysis of Neogene-Quaternary structures from seismic lines, surface measurements and geological-mapping is presented from the border zone between the Alps, Dinarides and Pannonian Basin. First, Early Miocene extension was possibly characterised by ENE directed extension. It was partly synchronous with NW-SE shortening. Second, Middle Miocene extension was possibly characterised by NW-SE to WNW-ESE directed extension. Again, this event was followed by a new generation of thrusts related to end-Sarmatian shortening. The last, Late Miocene E-W to WNW-ESE directed extension was followed by a final shortening that created major, map-scale folds, basement pop-ups and inverted former basins. Geometry, onlap and thickness patterns of the youngest syn-tectonic basin fill indicate that this last, N-S to NW-SE directed shortening started in Late Pontian and continued up to the present time. When taking into account the wider surrounding area, it seems that the structures related to this latest shortening are arranged in often perpendicular directions, centred at the eastern end of the Periadriatic lineament. To explain this fan-like pattern of synchronous shortenings a kinematic model is proposed combining counter-clockwise rotation with north- or northwestward shift of the Dinaridic block with respect to the more stable Alpine buttress. LA - English DB - MTMT ER - TY - JOUR AU - Vörös, Attila TI - Paleobiogeographical analysis: a tool for the reconstruction of Mesozoic Tethyan and Penninic basins JF - ACTA GEOLOGICA HUNGARICA: A QUARTERLY OF THE HUNGARIAN ACADEMY OF SCIENCES J2 - ACTA GEOL HUNG VL - 44 PY - 2001 IS - 2-3 SP - 145 EP - 158 PG - 14 SN - 0236-5278 UR - https://m2.mtmt.hu/api/publication/21052 ID - 21052 N1 - Cited By :11 Export Date: 23 February 2023 Correspondence Address: Vörös, A.; Department of Geology/Paleontology, P.O. Box 147, Budapest H-1431, Hungary LA - English DB - MTMT ER - TY - JOUR AU - Haas, János AU - P, Mioć AU - J, Pamić AU - B, Tomljenović AU - Árkai, Péter AU - A, Bérczi-Makk AU - Kovács, Sándor AU - B, Koroknai AU - E, Rálisch-Felgenhauer TI - Complex structural pattern of the Alpine-Dinaridic-Pannonian triple junction JF - INTERNATIONAL JOURNAL OF EARTH SCIENCES J2 - INT J EARTH SCI VL - 89 PY - 2000 IS - 2 SP - 377 EP - 389 PG - 13 SN - 1437-3254 DO - 10.1007/s005310000093 UR - https://m2.mtmt.hu/api/publication/1019043 ID - 1019043 N1 - Geological Research Group, Hungarian Academy of Sciences, Eötvös Lorand University, Muzeum krt. 4/a, H-1088 Budapest, Hungary Geological Survey of Slovenia, Dimiceva 14, SLO-1000 Ljubljana, Slovenia Croatian Academy of Sciences and Arts, Ante Kovacica 5, HR-10000 Zagreb, Croatia University of Zagreb, Pierollijeva 6, HR-10000 Zagreb, Croatia Laboratory for Geochemical Research, Hungarian Academy of Sciences, Budaorsi ul 45, H-1112 Budapest, Hungary MOL Hungarian Oil and Gas Co., Ballhyany u. 45, H-1039 Budapest, Hungary Hungarian Geological Institute, Stefdnia u. 14, H-1143 Budapest, Hungary Cited By :105 Export Date: 28 August 2023 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 - Márton Péterné Szalay, Emőke TI - The Tisza megatectonic unit in the light of paleomagnetic data JF - ACTA GEOLOGICA HUNGARICA: A QUARTERLY OF THE HUNGARIAN ACADEMY OF SCIENCES J2 - ACTA GEOL HUNG VL - 43 PY - 2000 IS - 3 SP - 329 EP - 343 PG - 15 SN - 0236-5278 UR - https://m2.mtmt.hu/api/publication/1155192 ID - 1155192 N1 - Cited By :45 Export Date: 25 March 2024 Correspondence Address: Márton, E.; Eotvos Lornd Inst. of Hungary, Columbus utca 17-23, Budapest H-1145, Hungary; email: h11000mar@ella.hu LA - English DB - MTMT ER - TY - CONF AU - Protic, L AU - Filipovic, I AU - Pelikán, P AU - Jovanovic, D AU - Kovács, Sándor AU - Sudar, M AU - Hips, Kinga AU - Less, György AU - Cvijic, R ED - Karamata, S ED - Jankovič, S TI - Correlation of the Carboniferous, Permian and Triassic sequences of the Jadar Block, Sana-Una and "Bükkium" Terranes T2 - Proceedings of the International Symposium Geology and Metallogeny of the Dinarides and the Vardar Zone PB - Academy of Sciences and Arts of the Republic of Srpska PY - 2000 SP - 61 EP - 69 PG - 9 UR - https://m2.mtmt.hu/api/publication/152208 ID - 152208 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 - Márton Péterné Szalay, Emőke AU - Pavelić, D AU - Tomljenović, B AU - Pamić, J AU - Márton, Péter TI - First palaeo-magnetic results on Tertiary rocks from the Slavonian Mountains in the southern Pannonian basin, Crotia JF - GEOLOGICA CARPATHICA J2 - GEOL CARPATH VL - 50 PY - 1999 SP - 273 EP - 279 PG - 7 SN - 1335-0552 UR - https://m2.mtmt.hu/api/publication/1042282 ID - 1042282 LA - English DB - MTMT ER - TY - JOUR AU - Márton Péterné Szalay, Emőke AU - Márton, Péter TI - Tectonic aspects of a palaeomagnetic study on the Neogene of the Mecsek Mountains JF - GEOFIZIKAI KÖZLEMÉNYEK - GEOPHYSICAL TRANSACTIONS J2 - GEOFIZIKAI KÖZLEMÉNYEK VL - 42 PY - 1999 SP - 159 EP - 180 PG - 22 SN - 0016-7177 UR - https://m2.mtmt.hu/api/publication/1042273 ID - 1042273 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 - B, Árgyelán G AU - Császár, Géza TI - Törmelékes krómspinellek a gerecsei jura képződményekben. JF - FÖLDTANI KÖZLÖNY J2 - FÖLDTANI KÖZLÖNY VL - 128 PY - 1998 IS - 2-3 SP - 321 EP - 360 PG - 40 SN - 0015-542X UR - https://m2.mtmt.hu/api/publication/20066690 ID - 20066690 LA - Hungarian DB - MTMT ER - TY - JOUR AU - Fodor, László AU - Jelen, B AU - Márton Péterné Szalay, Emőke AU - Skaberne, D AU - Čar, J AU - Vrabec, M TI - Miocene-Pliocene tectonic evolution of the Slovenian Periadriatic Line and surrounding area - Implications for Alpine-Carpathian extrusion models JF - TECTONICS J2 - TECTONICS VL - 17 PY - 1998 IS - 5 SP - 690 EP - 709 PG - 20 SN - 0278-7407 DO - 10.1029/98TC01605 UR - https://m2.mtmt.hu/api/publication/1155176 ID - 1155176 LA - English DB - MTMT ER - TY - JOUR AU - Frisch, W AU - Kuhlemann, J AU - Dunkl, István AU - Brügel, A TI - Palinspastic reconstruction and topographic evolution of the Eastern Alps during late Tertiary extrusion JF - TECTONOPHYSICS J2 - TECTONOPHYSICS VL - 297 PY - 1998 IS - 1-4 SP - 1 EP - 15 PG - 15 SN - 0040-1951 DO - 10.1016/S0040-1951(98)00160-7 UR - https://m2.mtmt.hu/api/publication/132435 ID - 132435 LA - English DB - MTMT ER - TY - CHAP AU - Kováč, M AU - Nagymarosy, András AU - Oszczypko, N AU - Csontos, L AU - Slaczka, A AU - Marunteanu, M AU - Matenco, L AU - Márton Péterné Szalay, Emőke ED - Rakús, M TI - Palinspastic reconstruction of the Carpathian - Pannonian region during the Miocene. T2 - Geodynamic development of the Western Carpathians PB - State Geological Institute of Dionýz Štúr CY - Pozsony SN - 8085314940 PY - 1998 SP - 189 EP - 217 PG - 29 UR - https://m2.mtmt.hu/api/publication/1155180 ID - 1155180 LA - English DB - MTMT ER - TY - JOUR AU - Márton Péterné Szalay, Emőke TI - The bending model of the Transdanubian Central Range (Hungary) in the light of Triassic palaeomagnetic data JF - GEOPHYSICAL JOURNAL INTERNATIONAL J2 - GEOPHYS J INT VL - 134 PY - 1998 IS - 2 SP - 625 EP - 633 PG - 9 SN - 0956-540X DO - 10.1046/j.1365-246x.1998.00598.x UR - https://m2.mtmt.hu/api/publication/1155168 ID - 1155168 N1 - Cited By :8 Export Date: 15 December 2023 Correspondence Address: Eotvos Lorand Geophys. Inst. Hung., Columbus utca 17-23, H-1145 Budapest, Hungary LA - English DB - MTMT ER - TY - JOUR AU - Vörös, Attila AU - Galácz, András TI - Jurassic palaeogeography of the Transdanubian Central Range (Hungary) JF - RIVISTA ITALIANA DI PALEONTOLOGIA E STRATIGRAFIA J2 - RIV IT PALEON STRATIG VL - 104 PY - 1998 IS - 1 SP - 69 EP - 84 PG - 16 SN - 0035-6883 DO - 10.13130/2039-4942/6112 UR - https://m2.mtmt.hu/api/publication/1021656 ID - 1021656 N1 - Cited By :64 Export Date: 25 March 2024 Correspondence Address: Vörös, A.; Department of Geology, Muzeum korut 14-16, H-1088 Budapest, Hungary AB - The Transdanubian Central Range (TCR) is a flattened range of hills in northern Transdanubia (Hungary), formed mainly by Mesozoic carbonate rocks showing strong facies similarities with the Southern Alps and the Austroalpine domain. The Jurassic system is divided into several formations of predominantly pelagic limestones. Ammonoids are frequent and were collected bed-by-bed in numerous sections, providing an excellent biostratigraphic resolution. The thickness of the Jurassic system is usually small but changes along the strike of the TCR. It reaches a maximum thickness of 500 m in the western part; is very variable (10-400 m) in the central segment (Bakony Mts.) and rather low (less than 100 m) in the east (Gerecse). In the Bakony segment, the thickness variation reflects the strongly dissected topography of the Jurassic sea-floor. Synsedimentary tectonics is dominated by normal faults; tilted blocks and listric faults may be inferred only in the east. Five main steps were identified in the palaeogeographic evolution: 1) Late Hettangian: carbonate oolitic shoals prevail, except for a few sites where non-deposition or neritic sediments occur. 2) Sinemurian and Pliensbachian: tectonic disintegration resulted in an intricate pattern of submarine horsts and intervening basins, with condensed sedimentation or non-deposition on the horsts and thicker, continuous sedimentary sequences in the basins. The submarine topographic highs are surrounded by aprons of redeposited material (scarp breccias, brachiopod coquinas, crinoida calcarenites, spiculitic cherry limestones), while pure or argillaceous limestones (Rosso Ammonitico) prevail in the distal areas. 3) Early Toarcian: the Tethys-wide anoxic event is superimposed on the previous submarine bottom topography; the resulting black shales and sedimentary Mn-ores are concentrated on the western sides of some horsts. 4) Dogger to Early Maim: radiolarites with heterochronous lower and upper boundaries (Aalenian to Kimmeridgian) prevail, except for the top of some submarine topographic highs. The absence of uppermost Bathonian to Lower Oxfordian carbonates suggests that the whole TCR sunk below the CCD in those times. 5) Latest Jurassic: the uniform deposition of Rosso Ammonitico and Biancone in the Late Kimmeridgian and Tithonian is interrupted only in the Early Tithonian by local intercalations of scarp breccias and coarse biodetrital limestones. This is interpreted as the last manifestation of synsedimentary tectonic movements along the faults bordering the submarine horsts. Based on palaeogeographic similarities and analogies in Jurassic times, the TCR is visualized as the northern foreground of the Trento platform/plateau (lying north of the later Insubric lineament), where the block-tectonic disintegration and differential subsidence started earlier and resulted in a bottom morphology more dissected than in the South Alpine part of this west Tethyan passive margin. LA - English DB - MTMT ER - TY - JOUR AU - Dunkl, István AU - Demény, Attila TI - Exhumation of the Rechnitz Window at the border of the Eastern Alps and Pannonian basin during Neogene extension. ALCAPA II Conference on Tectonics of the Alpine-Carpathian-Pannonian Region, COVASNA, ROMANIA, OCT 14-24, 1994 TS - ALCAPA II Conference on Tectonics of the Alpine-Carpathian-Pannonian Region, COVASNA, ROMANIA, OCT 14-24, 1994 JF - TECTONOPHYSICS J2 - TECTONOPHYSICS VL - 272 PY - 1997 IS - 2-4 SP - 197 EP - 211 PG - 15 SN - 0040-1951 DO - 10.1016/S0040-1951(96)00258-2 UR - https://m2.mtmt.hu/api/publication/1016488 ID - 1016488 LA - English DB - MTMT ER - TY - JOUR AU - Tari, Gábor AU - Dicea, O AU - Faulkerson, J AU - Georgiev, G AU - Popov, S AU - Stefanescu, M AU - Weir, G TI - Cimmerian and alpine stratigraphy and structural evolution of the moesian platform (Romania/Bulgaria) JF - AAPG MEMOIR J2 - AAPG MEMOIR VL - 68 PY - 1997 SP - 63 EP - 90 PG - 28 SN - 0271-8529 UR - https://m2.mtmt.hu/api/publication/32178175 ID - 32178175 LA - English DB - MTMT ER - TY - JOUR AU - Bada, G AU - Fodor, László AU - Székely, Balázs AU - Timár, Gábor TI - Tertiary brittle faulting and stress field evolution in the Gerecse Mountains, northern Hungary JF - TECTONOPHYSICS J2 - TECTONOPHYSICS VL - 255 PY - 1996 IS - 3-4 SP - 269 EP - 289 PG - 21 SN - 0040-1951 DO - 10.1016/0040-1951(95)00141-7 UR - https://m2.mtmt.hu/api/publication/1138169 ID - 1138169 AB - The Gerecse Mountains of the Transdanubian Range in northern Hungary have suffered polyphase deformation during the Tertiary. The evolution of the stress fields was determined by the detailed structural survey of the area: the statistical analysis of microtectonic observations, the mapping and reinterpretation of fault pattern and the study of basin stratigraphy and geometry. The stress fields show an apparent clockwise rotation from Eocene until Quaternary times. Three main phases were reconstructed. During the Eocene-Early Oligocene E-W- to ENE- WSW-oriented compression and perpendicular tension affected the area. The formation and evolution of several sedimentary basins were controlled by fault systems activated by this phase. After a period of intensive erosion in the Early Oligocene the stress field rotated approx, 30–40°: NW-SE-directed compression and NE- SW-trending tension existed during the Late Oligocene and Early Miocene. After correction with palaeomagnetic data, an original Palaeogene σ1 orientation is deduced NNE-SSW, reflecting the collisional processes of Europe and the Apulian microplate. The Middle Miocene to Pliocene period was characterised mainly by extensional deformation: the direction of the minimal stress axis (σ3) varied between E-W and NW-SE. The characteristic clockwise rotation pattern of the Tertiary palaeostress fields in the Gerecse Mts. is explained by the combined effect of the regional stress field changes in the Carpatho-Pannonian region and the rotation of the North Pannonian Unit. LA - English DB - MTMT ER - TY - JOUR AU - Harangi, Szabolcs AU - Szabó, Csaba AU - Józsa, Sándor AU - Szoldán, Z AU - Árva-Sós, Erzsébet AU - Balla, Márta AU - Kubovics, Imre TI - Mesozoic igneous suites in Hungary: Implications for genesis and tectonic setting in the northwestern part of Tethys JF - INTERNATIONAL GEOLOGY REVIEW J2 - INT GEOL REV VL - 38 PY - 1996 IS - 4 SP - 336 EP - 360 PG - 25 SN - 0020-6814 DO - 10.1080/00206819709465339 UR - https://m2.mtmt.hu/api/publication/1412630 ID - 1412630 N1 - Department of Petrology and Geochemistry, Eötvös University, Múzeum krt. 4/A, Budapest, 1088, Hungary Department of Isotope Analysis, Institute of Nuclear Research, Hungarian Academy of Sciences, Debrecen, Bern tér, 18c 4001, Hungary Institute of Nuclear Technology, Technical University, Budapest, 1521, Hungary Department of Petrology and Geochemistry, Eötvös University, Múzeum krt. 4/A, Budapest, 1088, Hungary Cited By :66 Export Date: 17 January 2023 AB - Mesozoic igneous rocks occur in various tectonic units of the Intra-Carpathian Area of Eastern Europe. These rocks were situated several hundred km apart from one another during their formation, and subsequent large lateral displacements resulted in their present positions. They formed during a relatively wide temporal range (Middle Triassic to Late Cretaceous) through different petrogenetic processes associated with the Mesozoic evolution of the northwestern part of Tethys. In the Transdanubian subunit of the Alcapa block, Middle Triassic calc-alkaline, intermediateto-acidic, and potassic rocks occur as pyroclastics, lava flows, and dikes in the Bakony and Buda mountains. The Gemer-Bükk subunit of the Alcapa block comprises two different igneous series: (1) slightly metamorphosed Middle Triassic volcanic rocks of the Eastern Bükk Mountains, which can be divided into an older (Anisian-Early Ladinian) calc-alkaline, intermediateto-acidic volcanic series and a younger (Late Ladinian) alkaline basaltic series; and (2) two series of the Middle Triassic to Middle Jurassic ophiolite complex (Bódva Magmatic Series and Darnó-Szarvaskö Magmatic Series), embedded in a tectonic mélange and in an olistostrome suite along a SW-NE-oriented zone. The Tisza block contains Early Cretaceous alkaline volcanic rocks in the Mecsek-Alföld subunit. Strong temporal and geochemical correlations have been observed between the Middle Triassic volcanic rocks of the Bakony and Buda mountains and the Southern Alps, and those of the Eastern Bükk Mountains and the Outer Dinarides. We propose that all these rocks were formed during the same extension-related volcanic activity along the Southern Alps-Bakony and Buda mountains-Eastern Bükk Mountains-Dinarides region. The Middle Triassic-Middle Jurassic ultramafic-mafic igneous rocks of the Gemer-Bükk subunit can be correlated with the ophiolites of the Inner Dinarides. Geochemistry of the mafic rocks is consistent with an origin from an N-MORB and E-MORB source mantle. The Middle to Late Triassic ultramafic and mafic rocks of the Bódva and Darnó-Szarvaskö series could have originated along the mid-oceanic ridge system of the northwestern segment of the Vardar ocean (Meliaticum). The Middle Jurassic igneous rocks of the Darnó-Szarvaskö series could have corresponded to the opening of a backarc basin. Early Cretaceous alkaline volcanic rocks of the Mecsek-Alföld zone in the Tisza block formed as a result of continental rifting along the southern margin of the European plate. Two volcanic series - a mafic and a sodic group - were generated from an OIB-like asthenospheric mantle. Separation of the Tisza block from the European plate occurred contemporaneously with volcanic activity during the late Early Cretaceous. LA - English DB - MTMT ER - TY - JOUR AU - Lelkes-Felvari, G AU - Árkai, Péter AU - Sassi, FP AU - Balogh, Kadosa TI - Main Features of The Regional Metamorphic Events in Hungary: A Review JF - GEOLOGICA CARPATHICA J2 - GEOL CARPATH VL - 47 PY - 1996 IS - 4 SP - 257 EP - 270 PG - 14 SN - 1335-0552 UR - https://m2.mtmt.hu/api/publication/1098670 ID - 1098670 AB - The present paper reviews data concerning the crystalline basement of all tectonic units in Hungary. Their lithologic content, biostratigraphic data, metamorphic features and radiometric age data are presented and critically discussed. The effects of at least two regional metamorphic cycles have been definitely recognized, Alpine and Variscan, and some polymetamorphic situations suggest the possible existence of a third, older event. The following main events are distinguished: the Alpine, the Variscan and an early Variscan or pre-Variscan stage or event. Alpine metamorphism turns out to be more widespread than previously reported. The Alpine metamorphic grade ranges from subgreenschist to greenschist facies conditions, locally reaching the lower amphibolite facies. Low to medium pressure conditions have been generally ascertained for it, with local exceptions of high and transitional medium to high pressure conditions. The Variscan metamorphism has been detected in the majority of the pre-Permian rock sequences in Hungary. Its metamorphic grade covers the whole temperature field of metamorphism, up to anatectic conditions. The pressure conditions in the monometamorphi. Variscan low grade metapelites turn out to be low, related to a thermal gradient close to 40 degrees C/km. A pre-Alpine polymetamorphic character is displayed by some Variscan amphibolite facies metapelites. The youngest mineral assemblages in them are characterized by the occurrence of andalusite in the rocks of suitable bulk composition, displaying a low-pressure character of the Variscan event, consistently with the above reported pressure estimate inferred from the greenschist facies monometamorphic metapelites. The oldest mineral assemblage is characterized by the occurrence of kyanite in rocks of suitable bulk composition, which may be either referred to an early Variscan stage or to a pre-Variscan event. LA - English DB - MTMT ER - TY - CHAP AU - Márton Péterné Szalay, Emőke AU - Márton, Péter ED - Morris, A and Tarling DH TI - Large scale rotations in North Hungary during the Neogene as indicated by palaeomagnetic data T2 - Palaeomagnetism and Tectonics of the Mediterranean Region PB - Geological Society of London CY - London T3 - Geological Society Special Publication, ISSN 0305-8719 ; 105. PY - 1996 SP - 153 EP - 173 PG - 21 UR - https://m2.mtmt.hu/api/publication/1057109 ID - 1057109 LA - English DB - MTMT ER - TY - JOUR AU - Árkai, Péter AU - Balogh, Kadosa AU - Dunkl, István TI - Timing of low-temperature metamorphism and cooling of the Paleozoic and Mesozoic formations of the Bükkium, innermost Western Carpathians, Hungary JF - GEOLOGISCHE RUNDSCHAU J2 - GEOL RUNDSCH VL - 84 PY - 1995 IS - 2 SP - 334 EP - 344 PG - 11 SN - 0016-7835 DO - 10.1007/BF00260444 UR - https://m2.mtmt.hu/api/publication/1098522 ID - 1098522 LA - English DB - MTMT ER - TY - JOUR AU - Fodor, László TI - FROM TRANSPRESSION TO TRANSTENSION - OLIGOCENE MIOCENE STRUCTURAL EVOLUTION OF THE VIENNA BASIN AND THE EAST ALPINE WESTERN CARPATHIAN JUNCTION JF - TECTONOPHYSICS J2 - TECTONOPHYSICS VL - 242 PY - 1995 IS - 1-2 SP - 151 EP - 182 PG - 32 SN - 0040-1951 DO - 10.1016/0040-1951(94)00158-6 UR - https://m2.mtmt.hu/api/publication/1368438 ID - 1368438 LA - English DB - MTMT ER - TY - JOUR AU - Haas, János AU - Kovács, Sándor AU - Krystyn, L AU - Lein, R TI - Significance of Late Permian-Triassic facies zones in terrane reconstructions in the Alpine-North Pannonian domain JF - TECTONOPHYSICS J2 - TECTONOPHYSICS VL - 242 PY - 1995 IS - 1-2 SP - 19 EP - 40 PG - 22 SN - 0040-1951 DO - 10.1016/0040-1951(94)00157-5 UR - https://m2.mtmt.hu/api/publication/1019016 ID - 1019016 N1 - Geological Research Group, the Hungarian Academy of Sciences, Múzeum krt. 4 / a, 1088 Budapest, Hungary University of Vienna, Department of Palaeontology, Universitätstr. 7, A-1010 Wien, Austria University of Vienna, Department of Geology, Universitätstr. 7, A-1010 Wien, Austria Cited By :245 Export Date: 28 August 2023 Correspondence Address: Haas, J.; Geological Research Group, the Hungarian Academy of Sciences, Múzeum krt. 4 / a, 1088 Budapest, Hungary AB - The present-day setting of the tectonic units (terranes) making up the pre-Neogene basement of the Pannonian Basin and the West Carpathians is the result of large-scale displacements during the Alpine collisional phases. To explain this setting, based on various concepts, a number of models have been proposed in the last decade. Most of them agree in an eastward escape of the ''North Pannonian terrane'' from the Alpine domain towards the Pannonian during the Palaeogene-Early Miocene period. In the present paper a reconstruction of the pre-escape setting of the displaced terranes is presented based on facies zones in selected time-slices from the Late Permian to the Late Triassic. According to our reconstruction the Inner West Carpathian units were located east of the Austroalpine units forming the northern shelf of the ''Euhallstatt''-Meliatic basin of the Vardar oceanic branch. The Drauzug should have been located in a position much more external than its present-day setting. The Transdanubian Range was situated in the northern neighbourhood of the Southern Alps, whereas the Bukk may have been located adjacent to the NW Dinarides. The Mid-Transdanubian zone is a major shear-zone containing elements of the Julian Alps and Sava folds nappe system and the Inner Dinaric ophiolitic melange. Although the nappe-tectonism may have played an important role in the structural evolution of the ''North Pannonian terrane'', this mechanism alone can hardly produce hundreds of kilometres of facies offset on the opposite sides of strike-slip zones. LA - English DB - MTMT ER - TY - JOUR AU - Haas, János AU - Budai, Tamás TI - Upper Permian-Triassic facies zones in the Transdanubian Range JF - RIVISTA ITALIANA DI PALEONTOLOGIA E STRATIGRAFIA J2 - RIV IT PALEON STRATIG VL - 101 PY - 1995 IS - 3 SP - 249 EP - 266 PG - 18 SN - 0035-6883 UR - https://m2.mtmt.hu/api/publication/1019017 ID - 1019017 LA - English DB - MTMT ER - TY - JOUR AU - Márton Péterné Szalay, Emőke AU - Fodor, László TI - Combination of palaeomagnetic and stress data - a case study from North Hungary. JF - TECTONOPHYSICS J2 - TECTONOPHYSICS VL - 242 PY - 1995 IS - 1-2 SP - 99 EP - 114 PG - 16 SN - 0040-1951 DO - 10.1016/0040-1951(94)00153-Z UR - https://m2.mtmt.hu/api/publication/1155117 ID - 1155117 N1 - Cited By :85 Export Date: 10 May 2023 Correspondence Address: Márton, E.; Eötvös Loránd Geophysical Institute of Hungary, Columbus u. 17-23, H-1145 Budapest XIV, Hungary LA - English DB - MTMT ER - TY - JOUR AU - Mauritsch, H AU - Márton Péterné Szalay, Emőke TI - Escape models of the Alpine-Carpathian-Pannonian region in the light of palaeomagnetic observations. JF - TERRA NOVA J2 - TERRA NOVA VL - 7 PY - 1995 IS - 1 SP - 44 EP - 50 PG - 7 SN - 0954-4879 DO - 10.1111/j.1365-3121.1995.tb00666.x UR - https://m2.mtmt.hu/api/publication/1155128 ID - 1155128 LA - English DB - MTMT ER - TY - JOUR AU - Neubauer, F AU - Dallmeyer, RD AU - Dunkl, István AU - Schirnik, D TI - Late Cretaceous exhumation of the metamorphic Gleinalm Dome, Eastern Alps: kinematics, cooling history, and sedimentary response in a sinistral wrench corridor JF - TECTONOPHYSICS J2 - TECTONOPHYSICS VL - 242 PY - 1995 SP - 79 EP - 98 PG - 20 SN - 0040-1951 DO - 10.1016/0040-1951(94)00154-2 UR - https://m2.mtmt.hu/api/publication/132359 ID - 132359 LA - English DB - MTMT ER - TY - JOUR AU - Császár, Géza AU - Árgyelán, GB TI - Stratigraphic and micromineralogic investigations on Cretaceous formations of the Gerecse Mountains, Hungary and their palaeogeographic implications JF - CRETACEOUS RESEARCH J2 - CRETACEOUS RES VL - 15 PY - 1994 IS - 4 SP - 417 EP - 434 PG - 18 SN - 0195-6671 DO - 10.1006/cres.1994.1024 UR - https://m2.mtmt.hu/api/publication/1447557 ID - 1447557 N1 - Cited By :30 Export Date: 26 March 2024 LA - English DB - MTMT ER - TY - JOUR AU - Kováč, M AU - Král', J AU - Márton Péterné Szalay, Emőke AU - Plašienka, D AU - Uher, P TI - Alpine uplift history of the Central Western Carpathians: geochronological, paleomagnetic, sedimantary and structural data. JF - GEOLOGICA CARPATHICA J2 - GEOL CARPATH VL - 45 PY - 1994 IS - 2 SP - 83 EP - 96 PG - 14 SN - 1335-0552 UR - https://m2.mtmt.hu/api/publication/1155109 ID - 1155109 LA - English DB - MTMT ER - TY - JOUR AU - M, Bleahu AU - Mantea, G AU - Bordea, S AU - Panin, S AU - Stefanescu, M AU - Sikic, K AU - Haas, János AU - Kovács, Sándor AU - Péró, Csaba AU - Bérczi-Makk, A AU - Konrád, Gyula AU - Nagy, E AU - Rálisch-Felgenhauer, E AU - Török, Ákos TI - Triassic facies types, evolution and paleogeographic relations of the Tisza Megaunit JF - ACTA GEOLOGICA HUNGARICA: A QUARTERLY OF THE HUNGARIAN ACADEMY OF SCIENCES J2 - ACTA GEOL HUNG VL - 37 PY - 1994 SP - 187 EP - 234 PG - 48 SN - 0236-5278 UR - https://m2.mtmt.hu/api/publication/1025533 ID - 1025533 LA - English DB - MTMT ER - TY - JOUR AU - Horváth, Ferenc TI - TOWARDS A MECHANICAL MODEL FOR THE FORMATION OF THE PANNONIAN BASIN JF - TECTONOPHYSICS J2 - TECTONOPHYSICS VL - 226 PY - 1993 IS - 1-4 SP - 333 EP - 357 PG - 25 SN - 0040-1951 DO - 10.1016/0040-1951(93)90126-5 UR - https://m2.mtmt.hu/api/publication/1255446 ID - 1255446 AB - New maps showing crustal and lithospheric thickness variations in the Pannonian basin and the surrounding East Alpine, Carpathian and Dinaric mountains have been prepared on the basis of recent seismic, seismologic and electromagnetic data. A map presenting Miocene faults of regional significance has been also constructed for the same region by using a wealth of recently available national and/or more local studies. It is suggested that observed crustal and lithospheric structural contrasts have been controlled primarily by Neogene kinematic history of the region. Kinematic history is characterized by the following main patterns: (1) indentation by Adria and large-scale backthrusting in the Southern Alps; (2) eastward escape and extension of the Eastern Alps; (3) extensional collapse in the Pannonian basin area; (4) formation of broad wrench fault systems along strike in the Dinarides and Southern Carpathians, and the Western Carpathians with dextral and sinistral shear, respectively; (5) compression and accretion of the external thrust and fold belt in the Eastern Carpathians. These kinematic patterns are thought to be interrelated and all are manifestations of the late-stage evolution of an overthickened orogenic wedge. In order to arrive at a better understanding of the mechanism of extension, which formed the Pannonian basin, deep crustal seismic profiles, hydrocarbon exploration reflection lines and borehole data have been analyzed in the Little Hungarian Plain. This plain represents the transition zone between the Alps and the Pannonian lowlands, and the results are illustrated by eight interpreted cross-sections. One result of regional importance is the clear recognition that the Transdanubian Central Range at the southeastern flank of the Little Hungarian Plain is composed of Alpine (pre-Senonian) thrust sheets. This finding marks the end of a century of debate: the allochthony of the substrata of the Pannonian basin can be now considered proven. Another result of more general interest is that these cross-sections document the mode of lithospheric extension. Preexisting compressional detachment planes reactivate as low-angle normal faults and lead to tectonic unroofing of deeply buried metamorphic terranes characterized by ductile flow along subhorizontal lineation. LA - English DB - MTMT ER - TY - JOUR AU - Márton Péterné Szalay, Emőke TI - The Itinerary of the Transdanubian Central Range: An assessment of relevant paleomagnetic observations. JF - ACTA GEOLOGICA HUNGARICA: A QUARTERLY OF THE HUNGARIAN ACADEMY OF SCIENCES J2 - ACTA GEOL HUNG VL - 37 PY - 1993 IS - 1-2 SP - 135 EP - 151 PG - 17 SN - 0236-5278 UR - https://m2.mtmt.hu/api/publication/1155104 ID - 1155104 LA - English DB - MTMT ER - TY - JOUR AU - Vörös, Attila TI - Jurassic microplate movements and brachiopod migrations in the western part of the Tethys JF - PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY J2 - PALAEOGEOGR PALAEOCL VL - 100 PY - 1993 IS - 1-2 SP - 125 EP - 145 PG - 21 SN - 0031-0182 DO - 10.1016/0031-0182(93)90037-J UR - https://m2.mtmt.hu/api/publication/21017 ID - 21017 N1 - Cited By :81 Export Date: 11 November 2022 CODEN: PPPYA Correspondence Address: Vörös, A.; Department of Geology and Paleontology, Hungarian Natural History Museum, Muzeum Körút 14-16, H-1370 Budapest, Hungary Funding details: Hungarian Scientific Research Fund, OTKA, 356/88 Funding text 1: The author is indebted to the organizerso f this special volume for inviting his paper. Special thanks are due to Dr. Miguel Mancefiido (La Plata) and to an anonymous reviewer for their valuable comments,a nd \\['ori mprovingthe English text. M. Mancefiido gave very important complementary data to the distributiono f Middle Jurassic nucleatids: Dr. M. Kfizm6r (Budapest) provided the author with a version of the tectonic base map used in Figs. 2 6. Their help is acknowledged herein. The present work was partly supported by the Hungarian Scientific Research Foundation (OTKA) Grant No. 356/88. AB - The paleobiogeography of the Jurassic brachiopods of the Alpine-Carpathian region and adjacent areas is discussed on the basis of the distribution of ''distinctive taxa''. The Jurassic microplates of the western part of Tethys and the present-day ''terranes'' of the Alpine-Carpathian region are outlined and their relationships are discussed. The migration possibilities of the brachiopods in the Jurassic Tethys were controlled mainly by plate/microplate movements and by changes in the oceanic current system. The Mediterranean microcontinent, isolated from the European and African shelves by oceanic/deep-sea belts, was the homeland of the Mediterranean brachiopod province. In the course of the Jurassic, the Mediterranean microcontinent moved, as part of the African plate, away from Europe, the widening Alboran-Ligurian-Penninic oceanic belt became a barrier preventing migration of brachiopods. By the end of the Middle Jurassic the Tisza microplate detached from Europe and formed a ''stepping stone'' for brachiopod dispersal. At about the same time, the ''Hesperian Strait'' opened between the basins of the Tethys and the Central Atlantic. The opening of this strait resulted in a reorganization of the Tethyan current system. The westward flowing equatorial currents which made a turn in the western corner of Tethys in the first half of the Mesozoic, now ran to the west through the Hesperian Strait via the Central Atlantic to the Pacific. This change produced a new pattern in brachiopod distribution: the Mediterranean fauna successfully invaded the European shelf, at the same time the Mediterranean province became impoverished. LA - English DB - MTMT ER - TY - JOUR AU - CSONTOS, L AU - Nagymarosy, András AU - Horváth, Ferenc AU - KOVAC, M TI - TERTIARY EVOLUTION OF THE INTRA-CARPATHIAN AREA - A MODEL JF - TECTONOPHYSICS J2 - TECTONOPHYSICS VL - 208 PY - 1992 IS - 1-3 SP - 221 EP - 241 PG - 21 SN - 0040-1951 DO - 10.1016/0040-1951(92)90346-8 UR - https://m2.mtmt.hu/api/publication/1255443 ID - 1255443 N1 - Eötvös University of Budapest, Department of Geology, 1088 Budapest, Múzeum krt. 4 / a, Hungary Eötvös University of Budapest, Department of Geophysics, 1082 Budapest, Ludovika tér 2, Hungary Slovakian Academy of Sciences, Department of Geology, 81473 Bratislava, Dúbravska cesta, Czechoslovakia Cited By :473 Export Date: 11 November 2022 Correspondence Address: Csontos, L. AB - The Outer Carpathian flysch nappes encircle an Intra-Carpathian domain which can be divided into two megatectonic units (North Pannonian and Tisza) mostly on the basis of contrasting Mesozoic and Palaeogene facies development. We see two major kinematic problems to be solved: (1) The present distribution of the Mesozoic and Palaeogene facies is mosaic-like, and some belts form exotic bodies within realms of Austroalpine affinity. (2) Late Eocene palinspastic reconstruction of the Outer Carpathian flysch nappes suggest, that the entire Intra-Carpathian area must have been located several hundreds of kilometres to the south and to the west of its present position. Neogene extension can account for shortening in the external Carpathian nappes, but is unable to explain Mesozoic facies anomalies and offsets of Palaeogene formations. We suggest that evolution of the Intra-Carpathian area involved first Late Palaeogene-Early Miocene juxtaposition of the North-Pannonian and Tisza megatectonic units, accompanied by the closure of the external Carpathian flysch troughs; thereafter extension of this amalgamated unit occurred, which was compensated by thrusting of flysch nappes onto the European foreland and formation of molasse foredeeps. Eastward escape of the North-Pannonian unit from the Alpine collisional belt involved left lateral shear along the Pieniny Klippen belt and right lateral shear along the Mid-Hungarian zone. Parts of the Late Palaeogene basin and an Early Miocene volcanic edifice were dissected, offset and elongated by several 100 kms. The driving mechanism of the eastward escape of the Intra-Carpathian area can be related to the collision of Apulia and Europe and the subduction of the external Carpathian crust under the Pannonian units. The escape ceased gradually in the Early Miocene, when oblique collision between the North-Pannonian unit and European continent occurred. Neogene extension of the Pannonian region was an areal deformation. The extension at locally variable rate resulted in the break-up of the heterogenous floor of the Neogene basin. The driving mechanism of basin extension and contemporaneous compressional deformation of the external Carpathians is thought to be related to ongoing subduction, involving the marginal part of the attenuated European continental crust. Tectonic activity in the Carpathians and basin subsidence and volcanism shifted in time and in unison from the west toward the east-southeast. LA - English DB - MTMT ER - TY - JOUR AU - Fodor, László AU - MAGYARI, A AU - Kázmér, Miklós AU - FOGARASI, A TI - GRAVITY-FLOW DOMINATED SEDIMENTATION ON THE BUDA PALEOSLOPE (HUNGARY) - RECORD OF LATE EOCENE CONTINENTAL ESCAPE OF THE BAKONY UNIT JF - GEOLOGISCHE RUNDSCHAU J2 - GEOL RUNDSCH VL - 81 PY - 1992 IS - 3 SP - 695 EP - 716 PG - 22 SN - 0016-7835 DO - 10.1007/BF01791386 UR - https://m2.mtmt.hu/api/publication/1368439 ID - 1368439 LA - English DB - MTMT ER - TY - JOUR AU - Márton Péterné Szalay, Emőke AU - Pagác, P AU - Túnyi, I TI - Paleomagnetic investigations on late Cretaceous-Cenozoic sediments from the NW part of the Pannonian Basin. JF - GEOLOGICA CARPATHICA J2 - GEOL CARPATH VL - 43 PY - 1992 IS - 6 SP - 363 EP - 368 PG - 6 SN - 1335-0552 UR - https://m2.mtmt.hu/api/publication/21057549 ID - 21057549 LA - English DB - MTMT ER - TY - JOUR AU - Szabó, Csaba AU - Harangi, Szabolcs AU - Csontos, László TI - REVIEW OF NEOGENE AND QUATERNARY VOLCANISM OF THE CARPATHIAN PANNONIAN REGION JF - TECTONOPHYSICS J2 - TECTONOPHYSICS VL - 208 PY - 1992 IS - 1-3 SP - 243 EP - 256 PG - 14 SN - 0040-1951 DO - 10.1016/0040-1951(92)90347-9 UR - https://m2.mtmt.hu/api/publication/1855796 ID - 1855796 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 - CATALANO, R AU - DISTEFANO, P AU - Kozur, Heinz TI - PERMIAN CIRCUMPACIFIC DEEP-WATER FAUNAS FROM THE WESTERN TETHYS (SICILY, ITALY) - NEW EVIDENCES FOR THE POSITION OF THE PERMIAN TETHYS JF - PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY J2 - PALAEOGEOGR PALAEOCL VL - 87 PY - 1991 IS - 1-4 SP - 75 EP - 108 PG - 34 SN - 0031-0182 DO - 10.1016/0031-0182(91)90131-A UR - https://m2.mtmt.hu/api/publication/1383045 ID - 1383045 AB - Circumpacific deep-water faunas, characterized mainly by radiolarians, paleopsychrospheric ostracods and conodonts, were found in the early, middle and late Permian deposits pertaining to the Sicanian paleogeographic domain of western Sicily, near the western end of the Eurasiatic Tethys. Similar Permian deep-water faunas are known from the Phyllite Unit of Crete and from Oman in the latter area partly above oceanic crust. All these occurrences indicate the presence of a late Paleozoic Tethys ocean immediately north of Gondwana. LA - English DB - MTMT ER - TY - JOUR AU - Árkai, Péter TI - Very low- and low-grade metamorphic rocks in the pre-Tertiary basement of the Drave Basin, SW-Hungary: mineral assemblages, illite crystallinity, b0 data, and problems of geological correlation JF - ACTA GEOLOGICA HUNGARICA: A QUARTERLY OF THE HUNGARIAN ACADEMY OF SCIENCES J2 - ACTA GEOL HUNG VL - 33 PY - 1990 IS - 1-3 SP - 43 EP - 67 PG - 25 SN - 0236-5278 UR - https://m2.mtmt.hu/api/publication/1114237 ID - 1114237 LA - English DB - MTMT ER - TY - JOUR AU - Dulai, Alfréd TI - The Lower Sinemurian (Jurassic) brachiopod fauna of the Lókút Hill (Bakony Mountains, Hungary). Preliminary results. JF - ANNALES HISTORICO-NATURALES MUSEI NATIONALIS HUNGARICI J2 - ANNLS HIST-NAT MUS NAT HUNG VL - 82 PY - 1990 SP - 25 EP - 37 PG - 13 SN - 0521-4726 UR - https://m2.mtmt.hu/api/publication/1072504 ID - 1072504 LA - English DB - MTMT ER - TY - JOUR AU - Márton Péterné Szalay, Emőke TI - Kinematics of the principal tectonic units of Hungary from paleomagnetic observations. JF - ACTA GEODAETICA GEOPHYSICA ET MONTANISTICA HUNGARICA J2 - ACTA GEOD GEOPHYS MONTAN HUNG VL - 25 PY - 1990 IS - 3-4 SP - 387 EP - 397 PG - 11 SN - 0236-5758 UR - https://m2.mtmt.hu/api/publication/1154968 ID - 1154968 LA - English DB - MTMT ER - TY - JOUR AU - Szente, István TI - Középső liász bivalviák paleobiogeográfiai értékelése az alp-kárpáti régióban. JF - ÁLTALÁNOS FÖLDTANI SZEMLE J2 - ÁLTALÁNOS FÖLDTANI SZEMLE VL - 25 PY - 1990 SP - 223 EP - 229 PG - 7 SN - 0133-6339 UR - https://m2.mtmt.hu/api/publication/2222072 ID - 2222072 LA - Hungarian DB - MTMT ER - TY - CHAP AU - Sztanó, Orsolya ED - Rosenfeld, R U TI - Submarine fan-channel conglomerate of Lower Cretaceous, Gerecse Mts., Hungary T2 - Neues Jahrbuch für Geologie und Paläontologie PB - E. Schweizerbart´sche Verlagsbuchhandlung CY - Stuttgart T3 - Monatshefte ; 7. PY - 1990 SP - 431 EP - 446 PG - 16 UR - https://m2.mtmt.hu/api/publication/1902908 ID - 1902908 LA - English DB - MTMT ER - TY - JOUR AU - Vörös, Attila AU - Horváth, Ferenc AU - Galácz, András TI - Triassic evolution of the Periadriatic margin in Hungary JF - BOLLETTINO DELLA SOCIETA GEOLOGICA ITALIANA J2 - BOLL SOC GEOL ITAL VL - 109 PY - 1990 SP - 73 EP - 81 PG - 9 SN - 0037-8763 UR - https://m2.mtmt.hu/api/publication/1021646 ID - 1021646 LA - English DB - MTMT ER - TY - JOUR AU - Árkai, Péter AU - Balogh, Kadosa TI - The age of metamorphism of the East Alpine-type basement, Little Plain, W-Hungary: K-Ar dating of K-white micas from very low- and low-grade metamorphic rocks JF - ACTA GEOLOGICA HUNGARICA: A QUARTERLY OF THE HUNGARIAN ACADEMY OF SCIENCES J2 - ACTA GEOL HUNG VL - 32 PY - 1989 IS - 1-2 SP - 131 EP - 147 PG - 17 SN - 0236-5278 UR - https://m2.mtmt.hu/api/publication/1114238 ID - 1114238 LA - English DB - MTMT ER - TY - CHAP AU - Kázmér, Miklós AU - Kovács, Sándor ED - ŞENGÖR, A M C TI - Triassic and Jurassic oceanic/paraoceanic belts in the Carpathian-Pannonian region and its surroundings. T2 - Tectonic Evolution of the Tethyan Region. PB - Kluwer Academic Publishers CY - Dordrecht PY - 1989 SP - 77 EP - 92 PG - 16 UR - https://m2.mtmt.hu/api/publication/1834233 ID - 1834233 LA - English DB - MTMT ER - TY - JOUR AU - Márton Péterné Szalay, Emőke AU - Márton, Péter TI - A compilation of palaeomagnetic results from Hungary JF - GEOFIZIKAI KÖZLEMÉNYEK - GEOPHYSICAL TRANSACTIONS J2 - GEOFIZIKAI KÖZLEMÉNYEK VL - 35 PY - 1989 SP - 117 EP - 133 PG - 17 SN - 0016-7177 UR - https://m2.mtmt.hu/api/publication/1054085 ID - 1054085 LA - English DB - MTMT ER - TY - JOUR AU - Haas, János AU - E, Rálisch-Felgenhauer AU - A, Oravecz-Scheffer AU - A, Bérczi-Makk AU - E, Nagy TI - Triassic key sections in the Mid-Transdanubian (Igal) structural zone JF - ACTA GEOLOGICA HUNGARICA: A QUARTERLY OF THE HUNGARIAN ACADEMY OF SCIENCES J2 - ACTA GEOL HUNG VL - 31 PY - 1988 SP - 3 EP - 18 PG - 16 SN - 0236-5278 UR - https://m2.mtmt.hu/api/publication/1019301 ID - 1019301 LA - English DB - MTMT ER - TY - JOUR AU - Kovács, S AU - Less, György AU - Piros, Olga AU - Róth, L TI - Az Aggtelek-Rudabányai-hegység triász formációi [Triassic formations of the Aggtelek-Rudabánya Mts.] JF - MAGYAR ÁLLAMI FÖLDTANI INTÉZET ÉVI JELENTÉSE J2 - M ÁLL FÖLDT INT JELENT VL - 1986 PY - 1988 SP - 19 EP - 43 PG - 25 SN - 0368-9751 UR - https://m2.mtmt.hu/api/publication/1311204 ID - 1311204 LA - English DB - MTMT ER - TY - GEN AU - Less, Gy AU - Grill, J AU - Szentpétery, Ildikó AU - Róth, L AU - Gyuricza, György ED - Less, Gy ED - Grill, J ED - Szentpétery, Ildikó TI - Az Aggtelek–Rudabányai-hegység fedetlen földtani térképe M = 1: 25.000 PY - 1988 UR - https://m2.mtmt.hu/api/publication/1996087 ID - 1996087 LA - Hungarian DB - MTMT ER - TY - JOUR AU - Haas, János TI - Position of the Transdanubian Central Range structural unit in the Alpine evolution phase JF - ACTA GEOLOGICA HUNGARICA: A QUARTERLY OF THE HUNGARIAN ACADEMY OF SCIENCES J2 - ACTA GEOL HUNG VL - 30 PY - 1987 SP - 243 EP - 256 PG - 14 SN - 0236-5278 UR - https://m2.mtmt.hu/api/publication/1019273 ID - 1019273 LA - English DB - MTMT ER - TY - JOUR AU - Horváth, Ferenc AU - Ádám, Antal AU - Stanley, WS TI - New geophysical data: evidence for the allochthony of the Transdanubian Central Range JF - RENDICONTI DELLA SOCIETA GEOLOGICA ITALIANA J2 - REND SOC GEOL ITAL VL - 9 PY - 1987 SP - 123 EP - 130 PG - 8 SN - 0392-3037 UR - https://m2.mtmt.hu/api/publication/1255424 ID - 1255424 LA - English DB - MTMT ER - TY - JOUR AU - Márton Péterné Szalay, Emőke TI - Paleomagnetism and tectonics in the Mediterranean region. JF - JOURNAL OF GEODYNAMICS J2 - J GEODYN VL - 7 PY - 1987 SP - 33 EP - 57 PG - 25 SN - 0264-3707 DO - 10.1016/0264-3707(87)90062-7 UR - https://m2.mtmt.hu/api/publication/1154348 ID - 1154348 N1 - Cited By :37 Export Date: 29 June 2022 Correspondence Address: Márton, E.; Eötvös Loránd Geophysical Institute of Hungary, 1145 Budapest, Hungary LA - English DB - MTMT ER - TY - JOUR AU - Ádám, O AU - Ráner, G AU - Haas, János TI - Az MK-1/82. geofizikai alapvonal Dabrony-Devecser közti szakaszának földtani értelmezése JF - MAGYAR ÁLLAMI EÖTVÖS LORÁND GEOFIZIKAI INTÉZET ÉVI JELENTÉSE = ANNUAL REPORT OF THE EOTVOS LORAND GEOPHYSICAL INSTITUTE OF HUNGARY J2 - MAGYAR ÁLLAMI EÖTVÖS LORÁND GEOFIZIKAI INT ÉVI JELENTÉSE VL - 1983 PY - 1985 SP - 117 EP - 121 PG - 5 SN - 0524-8655 UR - https://m2.mtmt.hu/api/publication/1019111 ID - 1019111 LA - Hungarian DB - MTMT ER - TY - JOUR AU - Galácz, András TI - Jurassic of Hungary: a review JF - ACTA GEOLOGICA HUNGARICA: A QUARTERLY OF THE HUNGARIAN ACADEMY OF SCIENCES J2 - ACTA GEOL HUNG VL - 27 PY - 1985 IS - 3-4 SP - 359 EP - 377 PG - 19 SN - 0236-5278 UR - https://m2.mtmt.hu/api/publication/1021617 ID - 1021617 LA - English DB - MTMT ER - TY - JOUR AU - Galácz, András AU - Horváth, Ferenc AU - Vörös, Attila TI - Sedimentary and structural evolution of the Bakony Mountains (Transdanubian Central Range, Hungary): paleogeographic implications JF - ACTA GEOLOGICA HUNGARICA: A QUARTERLY OF THE HUNGARIAN ACADEMY OF SCIENCES J2 - ACTA GEOL HUNG VL - 28 PY - 1985 IS - 1-2 SP - 85 EP - 100 PG - 16 SN - 0236-5278 UR - https://m2.mtmt.hu/api/publication/1021618 ID - 1021618 LA - English DB - MTMT ER - TY - JOUR AU - Kázmér, Miklós AU - KOVÁCS, Sándor TI - Permian-Paleogene paleogeography along the eastern part of the Insubric-Periadriatic lineament system: Evidence for continental escape of the Bakony-Drauzug unit. JF - ACTA GEOLOGICA HUNGARICA: A QUARTERLY OF THE HUNGARIAN ACADEMY OF SCIENCES J2 - ACTA GEOL HUNG VL - 28 PY - 1985 IS - 1-2 SP - 71 EP - 84 PG - 14 SN - 0236-5278 UR - https://m2.mtmt.hu/api/publication/1834167 ID - 1834167 LA - English DB - MTMT ER - TY - JOUR AU - Brezsnyánszky, Károly AU - Haas, János TI - A szenon nekézsenyi konglomerátum formáció sztratotípus szelvényének szedimentológiai és tektonikai vizsgálata JF - FÖLDTANI KÖZLÖNY J2 - FÖLDTANI KÖZLÖNY VL - 114 PY - 1984 IS - 1 SP - 81 EP - 100 PG - 20 SN - 0015-542X UR - https://m2.mtmt.hu/api/publication/1019097 ID - 1019097 LA - Hungarian DB - MTMT ER - TY - JOUR AU - Árkai, Péter TI - Very low- and low-grade Alpine regional metamorphism of the paleozoic and mesozoic formations of the Bükkium, NE-Hungary JF - ACTA GEOLOGICA HUNGARICA: A QUARTERLY OF THE HUNGARIAN ACADEMY OF SCIENCES J2 - ACTA GEOL HUNG VL - 26 PY - 1983 IS - 1-2 SP - 83 EP - 101 PG - 19 SN - 0236-5278 UR - https://m2.mtmt.hu/api/publication/1114268 ID - 1114268 LA - English DB - MTMT ER - TY - JOUR AU - Horváth, Ferenc AU - Royden, L TI - Mechanism for the formation of the intra-Carpathian basins: a review JF - EARTH EVOLUTION SCIENCES J2 - EARTH EVOL SCI VL - 1 PY - 1981 SP - 307 EP - 316 PG - 10 SN - 1881-8463 UR - https://m2.mtmt.hu/api/publication/1255403 ID - 1255403 LA - English DB - MTMT ER - TY - JOUR AU - Márton Péterné Szalay, Emőke AU - Márton, Péter TI - A Dunántúli-középhegység és a Villányi-hegység mezozoós paleopólusainak eltérésérõl JF - MAGYAR GEOFIZIKA J2 - MAGYAR GEOFIZIKA VL - 19 PY - 1978 SP - 129 EP - 136 PG - 8 SN - 0025-0120 UR - https://m2.mtmt.hu/api/publication/1041921 ID - 1041921 LA - Hungarian DB - MTMT ER - TY - JOUR AU - Vörös, Attila TI - Provinciality of the Mediterranean Lower Jurassic brachiopod fauna: causes and plate tectonic implications JF - PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY J2 - PALAEOGEOGR PALAEOCL VL - 21 PY - 1977 IS - 1 SP - 1 EP - 16 PG - 16 SN - 0031-0182 DO - 10.1016/0031-0182(77)90002-5 UR - https://m2.mtmt.hu/api/publication/20954 ID - 20954 N1 - Cited By :52 Export Date: 11 November 2022 CODEN: PPPYA Correspondence Address: Vörös, A.; Department of Geology and Palaeontology, Hungarian Natural History Museum, Budapest, Hungary LA - English DB - MTMT ER - TY - JOUR AU - CHANNELL, JET AU - Horváth, Ferenc TI - AFRICAN-ADRIATIC PROMONTORY AS A PALEO-GEOGRAPHICAL PREMISE FOR ALPINE OROGENY AND PLATE MOVEMENTS IN CARPATHO-BALKAN REGION JF - TECTONOPHYSICS J2 - TECTONOPHYSICS VL - 35 PY - 1976 IS - 1-3 SP - 71 EP - 101 PG - 31 SN - 0040-1951 DO - 10.1016/0040-1951(76)90030-5 UR - https://m2.mtmt.hu/api/publication/1255393 ID - 1255393 LA - English DB - MTMT ER -