Fault plane solutions of the January 26th, 2001 Bhuj earthquake sequence

Journal of Earth system science

S G Gaonkar2¹  J R Kayal4⁴  Reena De1²  Sagina Ram4⁴  B V Srirama3³ 

[1] Geological Survey of India, Central Region, Nagpur 440 006, India.$$;Geological Survey of India, Eastern Region, Salt Lake, Calcutta 700 091, India.$$;Geological Survey of India, Northern Region, Lucknow 226 024, India.$$;Geological Survey of India, 27, J. L. Nehru Road, Calcutta 700 016, India.$$

关键词: Bhuj;    mainshock;    aftershocks;    fault-plane solution;    reverse faulting.;   

DOI  :  

学科分类：天文学(综合)

来源: Indian Academy of Sciences

【 摘 要 】

A 12-station temporary microearthquake network was established by the Geological Survey of India for aftershock monitoring of the January 26th, 2001 Bhuj earthquake (𝑀W 7.6) in the Kutch district of Gujarat state, western India. The epicentres of the aftershocks show two major trends: one in the NE direction and the other in the NW direction. Fault-plane solutions of the best- located and selected cluster of events that occurred along the NE trend, at a depth of 15-38 km, show reverse faulting with a large left-lateral strike-slip motion, which are comparable with the main-shock solution. The NW trending upper crustal aftershocks at depth < 10 km, on the other hand, show reverse faulting with right-lateral strike-slip motion, and the mid crustal and lower crustal aftershocks, at a depth of 15-38 km, show pure reverse faulting as well as reverse faulting with right-lateral and left-lateral strike-slip motions; these solutions are not comparable with the main-shock solution. It is inferred that the intersection of two faults has been the source area for stress concentration to generate the main shock and the aftershocks.

【 授权许可】

Unknown