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The geodynamic evolution of the study area, restored from numerous well section data, demonstrates increased tectonic and basin subsidence during Late Permian-Early Triassic, Late Triassic and Early Jurassic rifting phases as well as after Mid-Cimmerian compression. There is a distinct trend for higher burial rates and depths of sediments from central southern part of the Moesian Platform to the south towards the Balkan orogenic system. Although the extensional processes are very important for the tectonic subside...