Seismic study and spatial observations of a & b – values for the different earthquake hazard zones of India

IF 1 Q4 GEOSCIENCES, MULTIDISCIPLINARY
Narayanakumar Somasundaram, S. Somala, E. Rogozhin, S. Rodina
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Abstract

This paper study the recent seismicity in Earthquake hazard zones in India. A large historical earthquake event catalog to cover the period of 1900-2018, the parameters date, time, latitude, longitude, depth and magnitude has been used to calculating frequency-magnitude distribution (b-value) of seismic hazard zones in India. To convert different magnitude scales into a single moment magnitude scale, the general orthogonal regression relation is used. Gamma distribution used for variable corrections also de-clustering method has used for removal of any non-Poisson distribution. The Indian seismic hazard zones are divided into five major seismic sources zones. The seismicity is characterized by Gutenberg-Richter relation. The parameter ‘b’ of FMD and relationship have been determined for these five seismic zones having different vulnerability environment. The ‘b’ values ranges between 0.43 to 1.16. The difference between the b parameters and seismic hazard level from seismic zones II to V considered for the study of high seismo-tectonic complexity and crustal heterogeneity, the parameter ‘a’ value changes accordingly the seismicity of the regions. The lowest b-values found in seismic zone II. The highest FMD b-value has been found in the seismic zone IV. Such high seismicity b-values may be associated with high heterogeneity. In this high b-value predict the low strength in the crust as well as seismic instabilities of that zone. These observations recommend not suggesting the location of important projects like atomic power stations, hydroelectric power stations, neutrino observatory projects, satellite town projects.
印度不同地震危险区的地震研究和a&b值的空间观测
本文研究了印度地震危险区近年来的地震活动性。利用1900-2018年的大型历史地震事件目录,利用日期、时间、纬度、经度、深度和震级等参数计算了印度地震危险区的频率-震级分布(b值)。为了将不同的震级转换为单一的矩震级,采用了一般的正交回归关系。伽马分布用于变量校正,也使用去聚类方法去除任何非泊松分布。印度地震危险区被划分为五个主要震源区。地震活动性具有古腾堡-里希特关系的特征。对这5个不同易损性环境的地震带,确定了FMD参数b及其关系。b值的范围在0.43到1.16之间。考虑地震构造复杂性和地壳非均质性较高的II - V震区b参数与地震危险性等级的差异,参数a值随震区地震活动性的变化而变化。最低的b值出现在II震区。在IV震区发现了最高的FMD b值。如此高的地震活动性b值可能与高非均质性有关。在这个高b值中预测了地壳的低强度以及该区域的地震不稳定性。这些观察建议不要建议重要项目的位置,比如原子能发电站、水力发电站、中微子天文台项目、卫星城项目。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Iranian Journal of Earth Sciences
Iranian Journal of Earth Sciences GEOSCIENCES, MULTIDISCIPLINARY-
CiteScore
1.40
自引率
12.50%
发文量
0
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