@inbook{MTMT:1464155, title = {The Late Cretaceous continental vertebrate fauna from Iharkút, western Hungary: a review}, url = {https://m2.mtmt.hu/api/publication/1464155}, author = {Ősi, Attila and Makádi, László and Rabi, Márton and Szentesi, Zoltán and Botfalvai, Gábor and Gulyás, P}, booktitle = {Bernissart Dinosaurs and Early Cretaceous Terrestrial Ecosystems}, unique-id = {1464155}, year = {2012}, pages = {533-570}, orcid-numbers = {Ősi, Attila/0000-0003-2967-997X; Szentesi, Zoltán/0000-0002-7019-5478; Botfalvai, Gábor/0000-0002-5479-9036} } @article{MTMT:2182126, title = {Episodic sedimentation on a peri-Tethyan ridge through the Middle-Late Jurassic transition (Villany Mountains, southern Hungary)}, url = {https://m2.mtmt.hu/api/publication/2182126}, author = {Vörös, Attila}, doi = {10.1007/s10347-011-0287-8}, journal-iso = {FACIES}, journal = {FACIES}, volume = {58}, unique-id = {2182126}, issn = {0172-9179}, abstract = {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.}, year = {2012}, eissn = {1612-4820}, pages = {415-443} } @article{MTMT:1417445, title = {Tectonically-controlled Late Triassic and Jurassic sedimentary cycles on a peri-Tethyan ridge (Villány, southern Hungary).}, url = {https://m2.mtmt.hu/api/publication/1417445}, author = {Vörös, Attila}, doi = {10.1556/CEuGeol.52.2009.2.2}, journal-iso = {CENT EUR GEOL}, journal = {CENTRAL EUROPEAN GEOLOGY}, volume = {52}, unique-id = {1417445}, issn = {1788-2281}, year = {2009}, eissn = {1789-3348}, pages = {125-151} } @article{MTMT:32550094, title = {Triassic}, url = {https://m2.mtmt.hu/api/publication/32550094}, author = {Feist-Burkhardt, S and Götz, AE and Szulc, J and Borkhataria, R and Geluk, M and Haas, János and Hornung, J and Jordan, P and Kempf, O and Michalík, J and Nawrocki, J and Reinhardt, L and Ricken, W and Röhling, HG and Rüffer, T and Török, Ákos and Zühlke, R}, journal-iso = {CENTRAL EUROPE}, journal = {CENTRAL EUROPE}, volume = {2}, unique-id = {32550094}, issn = {1479-0963}, year = {2008}, eissn = {1745-8218}, pages = {749-821}, orcid-numbers = {Haas, János/0000-0003-0929-8889; Török, Ákos/0000-0002-5394-4510} } @article{MTMT:1236932, title = {Mesozoic plate tectonic reconstruction of the carpathian region}, url = {https://m2.mtmt.hu/api/publication/1236932}, author = {Csontos, L and Vörös, Attila}, doi = {10.1016/j.palaeo.2004.02.033}, journal-iso = {PALAEOGEOGR PALAEOCL}, journal = {PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY}, volume = {210}, unique-id = {1236932}, issn = {0031-0182}, abstract = {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.}, year = {2004}, eissn = {1872-616X}, pages = {1-56} } @article{MTMT:1019054, title = {Mesozoic evolution of the Tisza Mega-unit}, url = {https://m2.mtmt.hu/api/publication/1019054}, author = {Haas, János and Péró, Csaba}, doi = {10.1007/s00531-004-0384-9}, journal-iso = {INT J EARTH SCI}, journal = {INTERNATIONAL JOURNAL OF EARTH SCIENCES}, volume = {93}, unique-id = {1019054}, issn = {1437-3254}, year = {2004}, eissn = {1437-3262}, pages = {297-313}, orcid-numbers = {Haas, János/0000-0003-0929-8889} } @article{MTMT:1025533, title = {Triassic facies types, evolution and paleogeographic relations of the Tisza Megaunit}, url = {https://m2.mtmt.hu/api/publication/1025533}, author = {M, Bleahu and Mantea, G and Bordea, S and Panin, S and Stefanescu, M and Sikic, K and Haas, János and Kovács, Sándor and Péró, Csaba and Bérczi-Makk, A and Konrád, Gyula and Nagy, E and Rálisch-Felgenhauer, E and Török, Ákos}, journal-iso = {ACTA GEOL HUNG}, journal = {ACTA GEOLOGICA HUNGARICA: A QUARTERLY OF THE HUNGARIAN ACADEMY OF SCIENCES}, volume = {37}, unique-id = {1025533}, issn = {0236-5278}, year = {1994}, pages = {187-234}, orcid-numbers = {Haas, János/0000-0003-0929-8889; Török, Ákos/0000-0002-5394-4510} } @article{MTMT:20936, title = {A Villányi-hegység alsó és középső júra képződményeinek üledékföldtani vizsgálata}, url = {https://m2.mtmt.hu/api/publication/20936}, author = {Vörös, Attila}, journal-iso = {FÖLDTANI KÖZLÖNY}, journal = {FÖLDTANI KÖZLÖNY}, volume = {102}, unique-id = {20936}, issn = {0015-542X}, year = {1972}, eissn = {2559-902X}, pages = {12-28} }