Formation dynamics of fault-block structures in the eastern segment of the Baikal-Stanovoi seismic belt

摘要

The combined analysis of geological-geophysical characteristics of active faults, morphotectonic features of the relief, and data of satellite measurements and on seismicity in the southeastern Aldan-Stanovoi block (the eastern flank of the Olekma-Stanovoi seismotectonic zone) made it possible to reconstruct the kinematic development of recent falt-block structures with the defining conjugate systems of main seismogenerating faults located in the zone of dynamic influence of three major lithospheric plates: Eurasian, Amur, and Sea of Okhotsk.