geomorfГеоморфология и палеогеографияGeomorfologiya i Paleogeografiya2949-17892949-1797geomorf-2639Research ArticleНаучные сообщенияShort communicationsВзаимосвязь геотектонических движений, плотностной дифференциации и геотермического режима мантийно-коровых блоков на территории СССРInterrelation between neotectonics, differentiation by density and geothermal regime of mantle-crustal blocks at the territory of the USSRЗверевА. Т.ZverevA. T.Московский институт инженеров геодезии, аэрофотосъемки и картографииРоссия19861011202203Геоморфология7684Copyright © Зверев А.Т., 20222022Зверев А.Т.Zverev A.T.Данная работа распространяется под лицензией Creative Commons Attribution 4.0.This work is licensed under a Creative Commons Attribution 4.0 License.https://geomorphology.igras.ru/jour/article/view/2639

Correlation analysis of neotectonic movements rates differentiation according to density and geothermal regime of mantle-crustal blocks suggests the geodynamic processes to be based on thermodynamic ones, the latter induce a complex of associated processes. Tectonic processes rate and character as well as manifestation depend on thermodynamic processes and on the depth of their development, lithosphere's permeability, heat and mass transfer mechanism and thermal characteristics of the matter at depth. Various combinations of the factors control the variety and development of tectonic processes (neotectonic crustal movements included) an different layers.

Correlation analysis of neotectonic movements rates differentiation according to density and geothermal regime of mantle-crustal blocks suggests the geodynamic processes to be based on thermodynamic ones, the latter induce a complex of associated processes. Tectonic processes rate and character as well as manifestation depend on thermodynamic processes and on the depth of their development, lithosphere's permeability, heat and mass transfer mechanism and thermal characteristics of the matter at depth. Various combinations of the factors control the variety and development of tectonic processes (neotectonic crustal movements included) an different layers.

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The authors declare that there are no conflicts of interest present.