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DISTRIBUTION OF CRETACIC / MIOCENE PETROFACIES AT THE CONTACT OF THE CARPATHIAN OROGENE AND MOLDAVIAN PLATFORM. MORPHOMETRIC PARTICULARITIES OF THE MOUNTAIN-PLATEAU RELIEF TRANSITION, BETWEEN SUCEAVA AND MOLDOVA VALLEY (OBCINA MARE/SUCEAVA PLATEAU, ROMANIA)
(STEF92 Technology, 2019-06-20, Doru-Toader Juravle)
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The geotectonic events in Late Cretaceous - Early Paleogene interval, caused essential changes in the architecture of the Tethysian paleogenic sedimentation basins and their rela relationship with the continental source areas. Laramic tectogenetic paroxysm (Maastrich tian/Danian) due to the subductin of the East European craton under the TiszaTisza-Dacia block, plays a double role in the structuralization of the East Carpathian units. In an internal position, the External Dacides are built (The Black Flysch, Barao...
Ecology and Environmental Protection2019