гравітаційний напружений стан

The method of the research relates to the field tectonophysics. The study of tectonic stress has always been the most important task of tectonic research. You can say that Tectonophysics began to flourish after the mass measurement of stress in-situ methods in mining and creation of stress reconstruction algorithm in natural geological data sets of slip faults. Data Mining showed a large predominance of horizontal compression environments in the areas of uplift and shields, and the prevalence of certain environments the horizontal extension in the crust basins and plates.

The method of the research relates to the theoretical tectonophysics. We study the question of the sources of energy of tectonic processes in the crust and lithosphere. They is divided into internal and external. Internal sources include the processes associated with the inversion density created during sedimentation in horizontally stratified array, as well as resulting from thermal heating due to the approach to the base of the lithosphere of the anomalous mantle.