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作者机构:Natl Geophys Res Inst CSIR Hyderabad 500007 Andhra Pradesh India
出 版 物:《CURRENT SCIENCE》 (Curr. Sci.)
年 卷 期:2013年第105卷第11期
页 面:1598-1604页
核心收录:
基 金:J.C. Bose Fellowship from DST, New Delhi DST
主 题:Earthquake nucleation micro-earthquakes short-term prediction
摘 要:We question the inferred downward nucleation of hypocentres that forms the basis for short-term earthquake prediction in the Koyna region. A careful relocation of foreshocks/aftershocks for a Mw 4.4 main shock sequence in 1996, hitherto believed to have occurred at 8 km depth, reveals that the main shock occurred at a depth of only 1.8 km, and formed part of a clear and almost instantaneous northward migration of micro-earthquakes along a narrow zone that could only be a fault plane at 4-8 km depth. This finding requires the current hypothesis for forecasting deep main shocks from shallow foreshocks in Koyna region to be discarded.