Глубинная скоростная структура в районе Улан-Удэ (восточное Прибайкалье)

Summary The authors determined the velocity structure from the Earth’s surface to a depth of 270 km around each point of observation in southern Siberia according to the P-receiver functions of broadband seismic stations. An example of the station Ulan-Ude (UUD) in East Baikal indicates that the velocity deep structure around the station can be graphically represented in the form of a specially designed circular model.