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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. 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"published" : false, "oldId" : 165562, "snippet" : true } ], "journal" : { "otype" : "Journal", "mtid" : 3558, "link" : "/api/journal/3558", "label" : "PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY 0031-0182 1872-616X", "pIssn" : "0031-0182", "eIssn" : "1872-616X", "reviewType" : "REVIEWED", "noIF" : false, "sciIndexed" : true, "scopusIndexed" : true, "lang" : "FOREIGN", "hungarian" : false, "published" : true, "oldId" : 3558, "snippet" : true }, "volume" : "210", "issue" : "1", "firstPage" : "1", "lastPage" : "56", "firstPageOrInternalIdForSort" : "1", "pageLength" : 56, "publishedYear" : 2004, "abstractText" : "Palaeomagnetic, palaeobiogeographic and structural comparisons of\ndifferent parts of the Alpine-Carpathian region suggest that four\nterranes comprise this area: the Alcapa, Tisza, Dacia and Adria\nterranes. These terranes are composed of different Mesozoic continental\nand oceanic fragments that were each assembled during a complex Late\nJurassic-Cretaceous Palaeogene history. Palaeomagnetic and tectonic\ndata suggest that the Carpathians are built up by two major oroclinal\nbends. The Alcapa bend has the Meliata oceanic unit, correlated with\nthe Dinaric Vardar ophiolite, in its core. It is composed of the\nWestern Carpathians, Eastern Alps and Southern Alcapa units\n(Transdanubian Range, Bukk). This terrane finds its continuation in the\nHigh Karst margin of the Dinarides. Further elements of the Alcapa\nterrane are thought to be derived from collided microcontinents:\nCzorsztyn in the N and a carbonate unit (Tisza?) in the SE. The\nTisza-Dacia bend has the Vardar oceanic unit in its core. It is\ncomposed of the Bihor and Getic microcontinents. This terrane finds its\ncontinuation in the Serbo-Macedonian Massif of the Balkans.\nThe Bihor-Getic microcontinent originally laid east of the Western\nCarpathians and filled the present Carpathian embayment in the Late\nPalaeozoic-Early Mesozoic. The Vardar ocean occupied an intermediate\nposition between the Western Carpathian-Austroalpine-Transdanubian-High\nKarst margin and the Bihor-Getic-Serbo-Macedonian microcontinent. The\nVardar and Pindos oceans were opened in the heart of the\nMediterranean-Adriatic microcontinent in the Late Permian-Middle\nTriassic. Vardar subducted by the end of Jurassic, causing the\nBihor-Getic-Serbo-Macedonian microcontinent to collide with the\ninternal Dinaric-Western Carpathian margin.\nAn external Penninic-Vahic ocean tract began opening in the Early\nJurassic, separating the Austroalpine-Western Carpathian microcontinent\n(and its fauna) from the European shelf. Further east, the\nSeverin-Ceahlau-Magura also began opening in the Early Jurassic, but\nfinal separation of the Bihor-Getic ribbon (and its fauna) from the\nEuropean shelf did not take place until the late Middle Jurassic.\nThe Alcapa and the Tisza-Dacia were bending during the\nAlbian-Maastrichtian. The two oroclinal bends were finally opposed and\npushed into the gates of the Carpathian embayment during the Palaeogene\nand Neogene. At that time, the main NS shortening in distant Alpine and\nHellenic sectors was linked by a broader right-lateral shear zone along\nthe former Vardar suture. (C) 2004 Elsevier B.V. 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