Seismic b-value anomalies prior to the 3rd January 2016, Mw=6.7 Manipur earthquake of northeast India

被引:28
作者
Borgohain, Jayanta Madhab [1 ,3 ]
Borah, Kajaljyoti [2 ]
Biswas, Rajib [3 ]
Bora, Dipok K. [1 ]
机构
[1] Diphu Govt Coll, Dept Phys, Karbi Anglong 782462, Assam, India
[2] Indian Inst Sci Educ & Res, Dept Earth Sci, Mohanpur 741246, W Bengal, India
[3] Tezpur Univ, Dept Phys, Geophys Lab, Tezpur 784028, Assam, India
关键词
b-value; Maximum likelihood method; Stress; Ludo-Myanmar subduction region; FREQUENCY-MAGNITUDE DISTRIBUTION; BURMESE ARC REGION; FRACTAL DIMENSION; MAGMA CHAMBERS; ALASKA; PLATEAU; COMPLETENESS; CATALOGS; VOLCANO; BENEATH;
D O I
10.1016/j.jseaes.2017.12.013
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Spatial variation of seismic b-value is estimated in the Indo-Myanmar subduction zone of northeast (NE) India using the homogeneous part of earthquake catalogue (1996-2015), recorded by International Seismological Center (ISC), consisting of 895 events of magnitude M-w >= 3.9. The study region is divided into 1 degrees x 1 degrees square grids and b-values are estimated at each grid by maximum likelihood method. In this study, the b-value varies from 0.75 to 1.54 in the region. Significant variation of low b-value in the respective location may indicate high stress accumulation in that region. Spatial variation reveals intermediate b-value anomalies around the epicenter of the M-w = 6/Manipur earthquake which occurred on 3rd January at 23:05 UTC (4 January 2016 at 04:35 IST). The variations of b-values are also estimated with respect to depth. The low b-value associated with the depth range similar to 15-55 km, which may imply crustal homogeneity and high stress accumulation in the crust. Since, NE India lies in the seismic zone V of the country; this study can be helpful to understand seismotectonics in the region.
引用
收藏
页码:42 / 48
页数:7
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