Spatio-temporal analysis of b-value prior to 28 April 2021 Assam Earthquake and implications thereof

被引:5
作者
Sharma, Vickey [1 ]
Bora, Dipok K. [2 ,3 ]
Biswas, Rajib [1 ]
机构
[1] Tezpur Univ, Dept Phys, Appl Geophys Lab, Tezpur 784028, India
[2] Diphu Govt Coll, Dept Phys, Karbi Anglong 782460, Assam, India
[3] Govt Model Coll, Karbi Anglon 782480, Assam, India
关键词
b; -value; Seismicity; Fault mechanisms; Stress; Seismotectonics; CALIFORNIA SEISMICITY; SPATIAL VARIATION; SHILLONG PLATEAU; NORTHEAST INDIA; KOPILI FAULT; MAGNITUDE; MOMENT; COMPLETENESS; STRESS; CATALOGS;
D O I
10.4401/ag-8802
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
Here, we report a Spatio-temporal analysis of the frequency magnitude distribution of earthquakes (b-value) before the 28th April 2021 (Mw 6.4) earthquake event observed in northeast India. To esti-mate the average b-value for the study region, a data set of 750 earthquake events with magnitude Mw >= 3.9 is extracted from the homogenous part of the earthquake catalog (1950-2021) documented by the United States Geological Survey (USGS) and International seismological center (ISC) in the region. For spatial analysis of the disparities in b-value, the whole study region is subdivided into 16 square grids of dimension 1ox1o and the b-value is calculated for each subsection. In congruence with other studies, this work yields b-values ranging from 0.66 to 1.25. After the calculation of the b-value for each grid, it is observed that the grid with the epicentral location of the 28th April 2021 (6.4) earthquake has a low b-value. Accordingly, the spatial correlation and aberrant pattern between b-value and focal depth have been comprehensively explored. It is observed that the b-value sig-nificantly dips within a depth range of similar to 15-35 km which implicates high-stress accumulation and crustal homogeneity. The depth-wise variation in b-value infers the antithetical relationship between b-value and crustal stress. Mostly interplate earthquakes are observed in the study region; thereby hinting at intense seismicity at the upper crust.
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