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Seismic b-Value and the Assessment of Ambient Stress in Northeast India

机译:印度东北部地震b值和环境应力评估

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Seismicity data of northeast India, recorded between 1986 and 1999 by a local network, are analysed for estimation of b -values. Based on the obtained values, viz. low (b ≤ 0.5), moderate (0.5 < b ≤ 0.7) and high (b > 0.7), the study area is classified into different seismic-domains. An assessment of stress level is also carried out in identifying seismic-domains. Seismic activities, though mostly confined in some sectors, are presumably triggered by mutual interaction of the Shillong Plateau, Mikir Hills, Indo-Burman Ranges and the easternmost part of the Himalayas, and the contributions from deep-seated fractures cannot be ignored. The results resemble the seismic character of a foreland setting adjacent to a convergent margin. The b -values estimated for 240 square grids of dimension 0.6° × 0.6° over five seismic domains indicate wide variation. An analysis of cumulative seismic moment release (M O) in different layers also indicates an anomaly in reference to the total seismic-energy budget of the five zones. The lower b -value and higher M O recorded at relatively lower depth (~30 km) towards the southwest of the study area might be associated with upward bulging of a strong lithosphere. The bulging is perhaps regionally compensated by the downward flexing of the descending Indian lithosphere beneath the Upper Assam area; features unequivocally observed in any foreland setup. Towards the north and east of the study area, random variations of in both b -value and M O along the converging zone suggest a varied tectonic environment with active interaction between the tectonic elements in these areas.
机译:分析印度东北部在1986年至1999年之间通过本地网络记录的地震数据,以估算b值。基于获得的值,即。低(b≤0.5),中(0.5 0.7),研究区域分为不同的地震域。在确定地震区域时也要进行应力水平评估。地震活动虽然主要局限于某些地区,但可能是由西隆高原,米克尔山丘,印度-布尔曼山脉和喜马拉雅山的最东部相互影响而引发的,深部裂缝的影响不容忽视。结果类似于邻近收敛边缘的前陆环境的地震特征。在五个地震域上对尺寸为0.6°×0.6°的240个正方形网格估计的b值表明变化很大。对不同层的累积地震矩释放量(M O)的分析也表明,相对于五个区域的总地震能量预算而言,这是一个异常。在向研究区西南部相对较低的深度(约30 km)处记录的较低的b值和较高的M O可能与强岩石圈的向上隆起有关。凸起可能是由上阿萨姆邦地区下方的下降的印度岩石圈的向下弯曲所补偿的。在任何前陆环境中都可以清晰观察到的特征。朝研究区的北部和东部,b值和M O沿收敛带的随机变化表明这些地区的构造环境之间存在活跃的相互作用,构成了变化的构造环境。

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