TY - CHAP AU - Ősi, Attila AU - Makádi, László AU - Rabi, Márton AU - Szentesi, Zoltán AU - Botfalvai, Gábor AU - Gulyás, P ED - Farlow, J TI - The Late Cretaceous continental vertebrate fauna from Iharkút, western Hungary: a review T2 - Bernissart Dinosaurs and Early Cretaceous Terrestrial Ecosystems PB - Indiana University Press CY - Indianapolis (IN) SN - 9780253357212 PY - 2012 SP - 533 EP - 570 PG - 38 UR - https://m2.mtmt.hu/api/publication/1464155 ID - 1464155 N1 - Cited By :40 Export Date: 15 December 2018 LA - English DB - MTMT ER - TY - JOUR AU - Vörös, Attila TI - Episodic sedimentation on a peri-Tethyan ridge through the Middle-Late Jurassic transition (Villany Mountains, southern Hungary) JF - FACIES J2 - FACIES VL - 58 PY - 2012 IS - 3 SP - 415 EP - 443 PG - 29 SN - 0172-9179 DO - 10.1007/s10347-011-0287-8 UR - https://m2.mtmt.hu/api/publication/2182126 ID - 2182126 N1 - Cited By :17 Export Date: 23 February 2023 Correspondence Address: Vörös, A.; Research Group for Paleontology, , Budapest, Ludovika tér 2, 1083, Hungary; email: voros@nhmus.hu AB - The Villany area, as a central part of the Tisza microcontinent/terrane along the European margin of Tethys, was characterized by intense subsidence in the Early and Middle Triassic, followed by a long interruption of subsidence in the Late Triassic to Middle Jurassic. During the Middle-Late Jurassic transition, marine sedimentation started with three distinct sedimentary episodes dated as Late Bathonian, Early Callovian, and Middle-Late Callovian, respectively. The succession is terminated by a thick limestone of Middle Oxfordian age. The sedimentary features, microfacies, and macroinvertebrate associations of these four stratigraphic units are documented and illustrated. The Middle to Late Jurassic sedimentary episodes of the Villany succession record an interplay of local and global factors and paleogeographical changes. At the beginning, local tectonic movements governed the main features of sedimentation, though the role of eustasy was also essential. From the mid-Callovian onwards, global climatic, biotic, and paleoceanographical changes controlled the nature and formation of the local carbonate sediments. The Callovian stromatolites are attributed to the activity of sulphate-reducing bacteria in a deep sublittoral, current-swept environment. Upwelling of eutrophic Tethyan waters is recorded by the prevalence of the Bositra filament microfacies in the Callovian. The long submarine hiatus at around the Callovian-Oxfordian transition mirrors a serious restriction of the carbonate budget, due to sudden cooling and a change in the oceanic current system (opening of a circumglobal Tethyan Passage), and to a higher amount of dissolved CO2. In the Middle Oxfordian, the carbonate production considerably increased in accordance with the sudden global warming. LA - English DB - MTMT ER - TY - JOUR AU - Vörös, Attila TI - Tectonically-controlled Late Triassic and Jurassic sedimentary cycles on a peri-Tethyan ridge (Villány, southern Hungary). JF - CENTRAL EUROPEAN GEOLOGY J2 - CENT EUR GEOL VL - 52 PY - 2009 IS - 2 SP - 125-151 SN - 1788-2281 DO - 10.1556/CEuGeol.52.2009.2.2 UR - https://m2.mtmt.hu/api/publication/1417445 ID - 1417445 N1 - megjelent: 2010-ben LA - English DB - MTMT ER - TY - JOUR AU - Feist-Burkhardt, S AU - Götz, AE AU - Szulc, J AU - Borkhataria, R AU - Geluk, M AU - Haas, János AU - Hornung, J AU - Jordan, P AU - Kempf, O AU - Michalík, J AU - Nawrocki, J AU - Reinhardt, L AU - Ricken, W AU - Röhling, HG AU - Rüffer, T AU - Török, Ákos AU - Zühlke, R TI - Triassic JF - CENTRAL EUROPE J2 - CENTRAL EUROPE VL - 2 PY - 2008 SP - 749 EP - 821 PG - 73 SN - 1479-0963 UR - https://m2.mtmt.hu/api/publication/32550094 ID - 32550094 N1 - Cited By :117 Export Date: 12 January 2023 LA - English DB - MTMT ER - TY - JOUR AU - Csontos, L AU - Vörös, Attila TI - Mesozoic plate tectonic reconstruction of the carpathian region JF - PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY J2 - PALAEOGEOGR PALAEOCL VL - 210 PY - 2004 IS - 1 SP - 1 EP - 56 PG - 56 SN - 0031-0182 DO - 10.1016/j.palaeo.2004.02.033 UR - https://m2.mtmt.hu/api/publication/1236932 ID - 1236932 N1 - Cited By :483 Export Date: 11 November 2022 CODEN: PPPYA Correspondence Address: Csontos, L.; Geological Department, Pazmany P: setany 1/a, Budapest 1117, Hungary; email: csontos@ludens.elte.hu Funding details: Hungarian Science Foundation, T 037595, T 043760 Funding text 1: The authors are indebted to many colleagues for the discussions of earlier oral and written versions of the manuscript. We would like to thank especially F. Horváth, A. Galácz, S. Kovács, M. Kázmér, E. Márton (Budapest), D. Plašienka, M. Kováč (Bratislava), F. Neubauer and Č. Tomek (Salzburg), K. Birkenmajer (Kraków), M. Săndulescu (Bucharest) S. Schmid (Basel) and P. Ziegler (Basel). We express our thanks to W. Frisch, F. Horváth, G. Stampfli, Alonso-Gutierrez, J. Von Raumer, B. Murphy, A. Collins and D. Nance who kindly revised and improved earlier versions of the manuscript. This version was helped by critical remarks of K. Birkenmajer, F. Neubauer, B. Sperner, G. Stampfli, and F. Surlyk. IGCP project 453 is gratefully thanked for moral and material support. Hungarian Science Foundation OTKA projects T 043760, T 037595 are also thanked for support. AB - Palaeomagnetic, palaeobiogeographic and structural comparisons of different parts of the Alpine-Carpathian region suggest that four terranes comprise this area: the Alcapa, Tisza, Dacia and Adria terranes. These terranes are composed of different Mesozoic continental and oceanic fragments that were each assembled during a complex Late Jurassic-Cretaceous Palaeogene history. Palaeomagnetic and tectonic data suggest that the Carpathians are built up by two major oroclinal bends. The Alcapa bend has the Meliata oceanic unit, correlated with the Dinaric Vardar ophiolite, in its core. It is composed of the Western Carpathians, Eastern Alps and Southern Alcapa units (Transdanubian Range, Bukk). This terrane finds its continuation in the High Karst margin of the Dinarides. Further elements of the Alcapa terrane are thought to be derived from collided microcontinents: Czorsztyn in the N and a carbonate unit (Tisza?) in the SE. The Tisza-Dacia bend has the Vardar oceanic unit in its core. It is composed of the Bihor and Getic microcontinents. This terrane finds its continuation in the Serbo-Macedonian Massif of the Balkans. The Bihor-Getic microcontinent originally laid east of the Western Carpathians and filled the present Carpathian embayment in the Late Palaeozoic-Early Mesozoic. The Vardar ocean occupied an intermediate position between the Western Carpathian-Austroalpine-Transdanubian-High Karst margin and the Bihor-Getic-Serbo-Macedonian microcontinent. The Vardar and Pindos oceans were opened in the heart of the Mediterranean-Adriatic microcontinent in the Late Permian-Middle Triassic. Vardar subducted by the end of Jurassic, causing the Bihor-Getic-Serbo-Macedonian microcontinent to collide with the internal Dinaric-Western Carpathian margin. An external Penninic-Vahic ocean tract began opening in the Early Jurassic, separating the Austroalpine-Western Carpathian microcontinent (and its fauna) from the European shelf. Further east, the Severin-Ceahlau-Magura also began opening in the Early Jurassic, but final separation of the Bihor-Getic ribbon (and its fauna) from the European shelf did not take place until the late Middle Jurassic. The Alcapa and the Tisza-Dacia were bending during the Albian-Maastrichtian. The two oroclinal bends were finally opposed and pushed into the gates of the Carpathian embayment during the Palaeogene and Neogene. At that time, the main NS shortening in distant Alpine and Hellenic sectors was linked by a broader right-lateral shear zone along the former Vardar suture. (C) 2004 Elsevier B.V. All rights reserved. LA - English DB - MTMT ER - TY - JOUR AU - Haas, János AU - Péró, Csaba TI - Mesozoic evolution of the Tisza Mega-unit JF - INTERNATIONAL JOURNAL OF EARTH SCIENCES J2 - INT J EARTH SCI VL - 93 PY - 2004 IS - 2 SP - 297 EP - 313 PG - 17 SN - 1437-3254 DO - 10.1007/s00531-004-0384-9 UR - https://m2.mtmt.hu/api/publication/1019054 ID - 1019054 N1 - Cited By :137 Export Date: 11 November 2022 CODEN: IJESF Correspondence Address: Haas, J.; Geological Research Group, , Budapest 1117, Hungary; email: haas@ludens.elte.hu Funding details: Hungarian Scientific Research Fund, OTKA, T037595 Funding details: Magyar Tudományos Akadémia, MTA Funding text 1: Acknowledgement This study was supported by the Hungarian Academy of Sciences and the Hungarian Scientific Research Fund (OTKA Project T037595) The authors thank Professor Stefan Schmid and S ndor Kov cs for helpful discussions and comments. We are much obliged to Professor Wolfgang Frisch and Professor Peter Faupl for their careful and constructive reviews. Authors are indebted to Henry Lieberman (Houston, USA) for the lingual corrections. 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 - Vörös, Attila TI - A Villányi-hegység alsó és középső júra képződményeinek üledékföldtani vizsgálata JF - FÖLDTANI KÖZLÖNY J2 - FÖLDTANI KÖZLÖNY VL - 102 PY - 1972 SP - 12 EP - 28 PG - 17 SN - 0015-542X UR - https://m2.mtmt.hu/api/publication/20936 ID - 20936 LA - Hungarian DB - MTMT ER -