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Information Journal Paper

Title

MESOZOIC PALEOGEOGRAPHY AND FACIES DISTRIBUTION IN THE NORTHERN MEDITERRANEAN TETHYS FROM WESTERN CARPATHIANS VIEW

Pages

  10-19

Abstract

 West Carpathian MESOZOIC paleogeographic development indicates the effect of a left lateral shift of the Alpine-Carpathian microcontinent along the European shelf since the Early Jurassic. The evolution during Late Triassic/Early Jurassic was controlled by convergence along the border of the Meliata Ocean and by contemporaneous divergence along the Middle Atlantic/Penninic rift. During Mid-Cretaceous, the convergence between Africa and Paleoeurope started, which finally resulted in collision of Alpine-West Carpathian microcontinent with the Paleoeuropean margin and in the formation of the Alpine Orogen.

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  • Cite

    APA: Copy

    MICHALIK, J.. (2011). MESOZOIC PALEOGEOGRAPHY AND FACIES DISTRIBUTION IN THE NORTHERN MEDITERRANEAN TETHYS FROM WESTERN CARPATHIANS VIEW. IRANIAN JOURNAL OF EARTH SCIENCES (IJES), 3(1), 10-19. SID. https://sid.ir/paper/326604/en

    Vancouver: Copy

    MICHALIK J.. MESOZOIC PALEOGEOGRAPHY AND FACIES DISTRIBUTION IN THE NORTHERN MEDITERRANEAN TETHYS FROM WESTERN CARPATHIANS VIEW. IRANIAN JOURNAL OF EARTH SCIENCES (IJES)[Internet]. 2011;3(1):10-19. Available from: https://sid.ir/paper/326604/en

    IEEE: Copy

    J. MICHALIK, “MESOZOIC PALEOGEOGRAPHY AND FACIES DISTRIBUTION IN THE NORTHERN MEDITERRANEAN TETHYS FROM WESTERN CARPATHIANS VIEW,” IRANIAN JOURNAL OF EARTH SCIENCES (IJES), vol. 3, no. 1, pp. 10–19, 2011, [Online]. Available: https://sid.ir/paper/326604/en

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