TY - JOUR AU - Hagdorn, H AU - Konrád, Gyula AU - Török, Ákos TI - Crinoids from the Muschelkalk of the Mecsek Mountains and their stratigraphic significance JF - ACTA GEOLOGICA HUNGARICA: A QUARTERLY OF THE HUNGARIAN ACADEMY OF SCIENCES J2 - ACTA GEOL HUNG VL - 40 PY - 1997 IS - 4 SP - 391 EP - 410 PG - 20 SN - 0236-5278 UR - https://m2.mtmt.hu/api/publication/1324007 ID - 1324007 N1 - Muschelkalkmuseum Ingelfingen, Germany Janus Pannonius University, Dept. of Physical Geography, Pécs, Hungary Budapest Technical University, Dept. of Engineering Geology, Budapest, Hungary Schlossstrasse 11, D-74653 Ingelfingen, Germany Ifjuság Urja 6, H-7601 Pécs, Hungary XI. Sztoczek u. 2, H-1521 Budapest, Hungary Cited By :21 Export Date: 18 June 2021 Correspondence Address: Hagdorn, H.Schlossstrasse 11, D-74653 Ingelfingen, Germany; email: encrinus@t-online.de LA - English DB - MTMT ER - TY - JOUR AU - Szente, István TI - Bivalve assemblages from the Middle Triassic Muschelkalk of the Mecsek Mts, South Hungary: An overview JF - ACTA GEOLOGICA HUNGARICA: A QUARTERLY OF THE HUNGARIAN ACADEMY OF SCIENCES J2 - ACTA GEOL HUNG VL - 40 PY - 1997 IS - 4 SP - 411 EP - 424 PG - 14 SN - 0236-5278 UR - https://m2.mtmt.hu/api/publication/2224128 ID - 2224128 N1 - Department of Palaeontology, Eötvös University, Budapest, Hungary Ludovika tér 2, H-1083 Budapest, Hungary Cited By :13 Export Date: 25 March 2024 Correspondence Address: Szente, I.Ludovika tér 2, H-1083 Budapest, Hungary LA - English DB - MTMT ER - TY - JOUR AU - Monostori, Miklós TI - Ostracods and charophytes from the Triassic Kantavár Formation, Mecsek Mts, Hungary JF - ACTA GEOLOGICA HUNGARICA: A QUARTERLY OF THE HUNGARIAN ACADEMY OF SCIENCES J2 - ACTA GEOL HUNG VL - 39 PY - 1996 IS - 3 SP - 311 EP - 317 PG - 7 SN - 0236-5278 UR - https://m2.mtmt.hu/api/publication/1467974 ID - 1467974 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 - 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 - 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 - 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 - Kázmér, Miklós TI - Tectonic units of Hungary: Their boundaries and stratigraphy (A bibliographic guide). JF - ANNALES UNIVERSITATIS SCIENTIARUM BUDAPESTINENSIS DE ROLANDO EÖTVÖS NOMINATAE - SECTIO GEOLOGICA J2 - ANN UNIV SCI BP R EÖTVÖS NOM SECT GEOL VL - 26 PY - 1986 SP - 45 EP - 120 PG - 76 SN - 0365-0634 UR - https://m2.mtmt.hu/api/publication/1834166 ID - 1834166 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 -