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. Several large scale geological events controlled the Dacian Basin inception. The Dacian Basin can be defined as the southern Carpathian Foredeeparea outlined after a long migration process, where the sediment accumulation was stimulated by the Carpathian orogenic climax and organized within a morphologically closed basin and in a Neogene Paratethys brackish-water ecosystem

THE IDENTITY OF A PARATETHYS BASIN. DACIAN BASIN CONFIGURATION - OUTCOME OF THE CARPATHIAN FOREDEEP ALONG-ARC MIGRATION