러시아ㆍ유라시아
연구정보
ABOUT THE WAVE MECHANISM OF ACTIVATION OF FAULTS IN SEISMIC ZONES OF THE LITHOSPHERE IN MONGOLIA
몽골 국외연구자료 기타 M. G. Mel’nikov (Institute of the Earth’s Crust, SB RAS, Irkutsk, Russia) Institute of the Earth's crust, Siberian Branch of RAS 발간일 : 2016-09-08 등록일 : 2016-09-08 원문링크
The study is focused on earthquake migrations along active faults in seismic zones of Mongolia. The earthquake migrations are interpreted as a result of the influence of deformational waves. Vector velocities and other parameters of the deformational waves are studied. Based on data from largescale maps, local faults are compared, and differences and similarities of parameters of waves related to faults of different ranks are described.
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