Abstract
New methods are proposed for registering deformation waves and assessing their phase (vector) velocities based on earthquake monitoring in dynamic influence areas of active faults. Active faults in Central Asia are classified on the basis of the vector velocities of deformation waves. The complex parameters of the presently active faults and the vector velocities of the deformation waves are used for the geodynamic zoning of Central Asia. Such an approach offers new opportunities for the more extensive investigation of the geodynamic characteristics of spacious intracontinental structures that were tectonically active in the Cenozoic.
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