Petrological Geodynamic Model for the Evolution of the Crystalline Basement of the Eastern Russian Plate

The east of the Russian plate is a typical platform area of Earth's crust. Geological, geophysical and seismic studies show active geodynamic processes within the region. Due to these active geodynamic processes, sub-horizontal tension is formed in the crystalline basement rocks. This leads to sub-horizontal displacements – “disruption” of large blocks of rocks which are associated with the occurrence of decompressed zones destruction.