About the Deep Earth's Crust Structure by Earthquake Hypocenters in the Region of Olkhon Island

Abstract

The aseismic structure identified by the analysis of seismicity in the region of Olkhon Island which is associated with the central part of the Shebarta complex, composed of metamorphic rocks. The effect of subsidence of the seismically active layer under Olkhon Island is observed, and it rises to the center of the Baikal depression.