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Seismicity Pattern Analysis in and around Shillong Great Earthquake of 1897

机译:1897年西隆大地震及其周围地区的地震活动模式分析

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The seismicity data of the last 50 years (1963-2012) of the region bounded by 89° - 93° E and 24° -28° N have been analyzed for understanding the seismic characteristics in and around Shillong great earthquake of 1897. The distribution of earthquakes for this period shows sporadic nature of seismic activity in the region. The study of earthquake frequency, the spatio-temporal patterns of seismicity, the focal depth distribution, and the energy release pattern during the period 1963-2012 considering the events with cut-off magnitude (mb ≥ 4.5) have revealed that the region is seismically active. It is observed that most of the seismicity over the Shillong region is associated with the Main Central Thrust, Main Boundary Thrust and Transverse faults. The earthquake occurrence pattern is non-uniform and mostly shallow and intermediate focus in nature. Further, it has been observed that there exists a non-uniform pattern of seismic energy release.The Himalayan Physics Year 5, Vol. 5, Kartik 2071 (Nov 2014)Page: 36-38
机译:为了了解1897年西隆大地震及其周围地区的地震特征,对89°-93°E和24°-28°N界定的区域最近50年(1963-2012)的地震数据进行了分析。这段时期的地震资料表明该地区地震活动是零星的。对1963-2012年期间地震频率,地震时空分布,震源深度分布和能量释放模式的研究,考虑了截止强度为(mb≥4.5)的事件,表明该地区是地震活动地区。活性。可以看出,西隆地区的大部分地震活动与主要中央逆冲断层,主要边界逆冲断层和横向断层有关。地震的发生方式是不均匀的,并且在自然界中主要是浅层和中层。此外,已经观察到存在一种不均匀的地震能量释放模式。《喜马拉雅物理学年鉴》第5卷,第1期。 5,Kartik 2071(2014年11月)页码:36-38

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