H.V. Sargsyan (ovash@yandex.ru), G.R. Abgaryan (ovash@yandex.ru), SH.A. Aramyan (shirak_gum@mail.ru), A.A. Gevorgyan (ani_gevorkjan@mail.ru)
Abstract
After the Spitak earthquake on December 7, 1988, the Bavrian earthquake on February 13, 22 hours
25 minutes local time, with a magnitude of MS= 5.4 and an intensity at the epicenter of 10=7 points, was the
second with such intensity, lasted quite a long time due to strong aftershocks.
Keywords: mainshock, aftershocks, isoseist map, focal mechanism.
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