TY - JOUR AU - M. Tóth, Tivadar TI - Geochemistry of the Görcsöny Ridge amphibolites (Tisza Unit, SW Hungary) and its geodynamic consequences JF - GEOLOGIA CROATICA J2 - GEOL CROAT VL - 67 PY - 2014 IS - 1 SP - 17 EP - 32 PG - 16 SN - 1330-030X DO - 10.4154/gc.2014.02 UR - https://m2.mtmt.hu/api/publication/2474971 ID - 2474971 N1 - Cited By :4 Export Date: 12 February 2021 Correspondence Address: Tóth, T. M.; Department of Mineralogy, Egyetem u. 2-6, H-6722 Szeged, Hungary; email: mtoth@geo.u-szeged.hu AB - in press LA - English DB - MTMT ER - TY - JOUR AU - Buda, György AU - Koller, F AU - Ulrych, J TI - Petrochemistry of Variscan granitoids of Central Europe: Correlation of Variscan granitoids of Tisia and Pelsonian Terranes with granitoids of Moldanubicum, Western Carpathian and Southern Alps. A review: part I. JF - ACTA GEOLOGICA HUNGARICA: A QUARTERLY OF THE HUNGARIAN ACADEMY OF SCIENCES J2 - ACTA GEOL HUNG VL - 47 PY - 2004 SP - 117 EP - 138 PG - 22 SN - 0236-5278 DO - 10.1556/AGeol.47.2004.2-3.3 UR - https://m2.mtmt.hu/api/publication/2808607 ID - 2808607 N1 - Cited By :21 Export Date: 16 June 2023 Correspondence Address: Buda, G.; Department of Mineralogy, Pázmány P. st. 1/A, H-1117 Budapest, Hungary; email: buda@ludens.elte.hu LA - English DB - MTMT ER - TY - JOUR AU - Klötzli, U AU - Buda, György AU - Skiöld, T TI - Zircon typology, geochronology and whole rock Sr-Nd isotope systematics of the Mecsek Mountain granitoids in the Tisia Terrane (Hungary) JF - MINERALOGY AND PETROLOGY J2 - MINER PETROL VL - 81 PY - 2004 IS - 1-2 SP - 113 EP - 134 PG - 22 SN - 0930-0708 DO - 10.1007/s00710-003-0026-0 UR - https://m2.mtmt.hu/api/publication/2808782 ID - 2808782 N1 - Cited By :38 Export Date: 25 March 2024 Correspondence Address: Klötzli, U.S.; Institute of Geological Sciences, Althanstrasse 14, A-1090 Vienna, Austria; email: urs.kloetzli@univie.ac.at LA - English DB - MTMT ER - TY - JOUR AU - Horváth, Péter AU - Kovacs, G AU - Szakmány, György TI - Eclogite and garnet amphibolite pebbles from Miocene conglomerates (Pannonian Basin, Hungary): Implications for the Variscan metamorphic evolution of the Tisza Megaunit JF - GEOLOGICA CARPATHICA J2 - GEOL CARPATH VL - 54 PY - 2003 IS - 6 SP - 355 EP - 366 PG - 12 SN - 1335-0552 UR - https://m2.mtmt.hu/api/publication/1004506 ID - 1004506 LA - English DB - MTMT ER - TY - JOUR AU - Raucsikné Varga, Andrea Beáta AU - Szakmány, György AU - Józsa, Sándor AU - Máthé, Zoltán TI - Petrology and geochemistry of Upper Carboniferous siliciclastic rocks (Téseny Sandstone Formation) from the Slavonian-Drava Unit (Tisza Megaunit, S Hungary) - summarized results JF - ACTA GEOLOGICA HUNGARICA: A QUARTERLY OF THE HUNGARIAN ACADEMY OF SCIENCES J2 - ACTA GEOL HUNG VL - 46 PY - 2003 IS - 1 SP - 95 EP - 113 PG - 19 SN - 0236-5278 DO - 10.1556/AGeol.46.2003.1.7 UR - https://m2.mtmt.hu/api/publication/1302285 ID - 1302285 N1 - Department of Petrology/Geochemistry, Eotvös Loránd Univ., Pazmany P. sétány 1/c, Budapest H-1117, Hungary Mecsek Ore Environment Company, Esztergár L. út 19, Pécs H-7633, Hungary Cited By :16 Export Date: 1 December 2023 Correspondence Address: Varga, A.R.; Department of Petrology/Geochemistry, Pazmany P. sétány 1/c, Budapest H-1117, 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 - 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 - 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 - Sudár Sándorné Svingor, Éva AU - Kovách, Ádám TI - Rb-Sr isotopic studies on granodioritic rocks from the Mecsek Mountains,Hungary. JF - ACTA GEOLOGICA HUNGARICA: A QUARTERLY OF THE HUNGARIAN ACADEMY OF SCIENCES J2 - ACTA GEOL HUNG VL - 24 PY - 1981 SP - 295 SN - 0236-5278 UR - https://m2.mtmt.hu/api/publication/1659720 ID - 1659720 N1 - [P03779] ATKI1981/0113 LA - English DB - MTMT ER -