Tectonic and lithologic structure of barguzinskiy rift southwest branch for the assessment the risk of dangerous natural processes in East Pribaikalye

Questions of neotectonic structure of East Pribaikalye and history of geological development in the late Cenozoic are considered. The neotectonic scheme of the region can form a basis for microseismic division into districts of the territory of Turkinskaya special economic zone. Sedimentary filling of the shallow hollows, which contours are predetermined by explosive violations, testifies to the long-lived history of their development, since Eopleistocene and to the present.