Геодинамика и тектонофизика (Sep 2015)

ABOUT THE WAVE MECHANISM OF ACTIVATION OF FAULTS IN SEISMIC ZONES OF THE LITHOSPHERE IN MONGOLIA

  • M. G. Mel’nikov

DOI
https://doi.org/10.5800/GT-2013-4-1-0092
Journal volume & issue
Vol. 4, no. 1
pp. 69 – 81

Abstract

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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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