Study of the epicentral trends and depth sections for aftershocks of the 26th January 2001, Bhuj earthquake in western India

Journal of Earth system science

J R Kayal4³  S G Gaonkar1¹  Reena De3⁴  B V Srirama1¹  D V Punekar1¹  Sagina Ram2²  S R Samaddar1¹ 

[1] Geological Survey of India(CR), Seminary Hills, Nagpur, 440 006, India.$$;Geological Survey of India(NR), Sector E, Aligunj, Lucknow, India.$$;Geological Survey of India(CGD), 27 J.N. Road, Kolkata, 700 016, India.$$;Geological Survey of India(ER), Karunamayee, Salt Lake, Kolkata, India.$$

关键词: Aftershocks;    Bhuj earthquake;    depth section;    epicentral trend;    MEQ network.;   

DOI  :  

学科分类：天文学(综合)

来源: Indian Academy of Sciences

【 摘 要 】

The Geological Survey of India (GSI) established a twelve-station temporary microearthquake (MEQ) network to monitor the aftershocks in the epicenter area of the Bhuj earthquake (𝑀w 7.5) of 26th January 2001. The main shock occurred in the Kutch rift basin with the epicenter to the north of Bhachao village, at an estimated depth of 25km (IMD). About 3000 aftershocks (𝑀d ≥ 1.0), were recorded by the GSI network over a monitoring period of about two and half months from 29th January 2001 to 15th April 2001. About 800 aftershocks (𝑀d ≥ 2.0) are located in this study. The epicenters are clustered in an area 60km × 30km, between 23.3°N and 23.6°N and 70°E and 70.6°E. The main shock epicenter is also located within this zone.Two major aftershock trends are observed; one in the NE direction and other in the NW direction. Out of these two trends, the NE trend was more pronounced with depth. The major NE-SW trend is parallel to the Anjar-Rapar lineament. The other trend along NW-SE is parallel to the Bhachao lineament. The aftershocks at a shallower depth (< 10 km) are aligned only along the NW-SE direction. The depth slice at 10km to 20km shows both the NE-SW trend and the NW-SE trend. At greater depth (20 km{38 km) the NE-SW trend becomes more predominant. This observation suggests that the major rupture of the main shock took place at a depth level more than 20 km; it propagated along the NE-SW direction, and a conjugate rupture followed the NW-SE direction.A N-S depth section of the aftershocks shows that some aftershocks are clustered at shallower depth ≤ 10km, but intense activity is observed at 15-38km depth. There is almost an aseismic layer at 10-15km depth. The activity is sparse below 38 km. The estimated depth of the main shock at 25km is consistent with the cluster of maximum number of the aftershocks at 20-38 km. A NW-SE depth section of the aftershocks, perpendicular to the major NE-SW trend, indicates a SE dipping plane and a NE-SW depth section across the NW-SE trend shows a SW dipping plane.The epicentral map of the stronger aftershocks 𝑀 ≥ 4.0 shows a prominent NE trend. Stronger aftershocks have followed the major rupture trend of the main shock. The depth section of these stronger aftershocks reveals that it occurred in the depth range of 20 to 38 km, and corroborates with a south dipping seismogenic plane.

【 授权许可】

Unknown