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Late palaeozoic to cenozoic evolution of the Black SeaSouthern Eastern Europe region: A view from the Russian platform

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A synthesis of the Late Palaeozoic to Cenozoic evolution of the Black Sea region and the southern parts of the East European Platform (EEP) is presented. During Carboniferous to Early Permian times the Cordillera-type Euxinus Orogen evolved along the southern margin of the EEP in response to progressive closure of the Rheic and Palaeotethys oceans and the accretion of Gondwana-derived continental terranes. | Late palaeozoic to cenozoic evolution of the Black SeaSouthern Eastern Europe region: A view from the Russian platform

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Testing alternative tectono-stratigraphic interpretations of the late palaeozoic−early mesozoic Karakaya complex in NW Turkey: Support for an accretionary origin related to northward subduction of palaeotethys

Late palaeozoic to cenozoic evolution of the Black SeaSouthern Eastern Europe region: A view from the Russian platform