A Review on the Mechanism of Reservoir-Induced Seismicity for Nepalese Context

U. R. Joshi, R. Maskey, K. R. Kafle
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引用次数: 1

Abstract

Over 90 cases of Reservoir Induced Seismicity have been recorded around the earth. The magnitude was varying from 3.0 to 6.3 on the Richter scale. A Reservoir Induced Seismicity (RIS) can increase the frequency of earthquakes in seismically active zones and cause a shock in seismically inactive zones. Nepal is situated in a seismically active zone with six large earthquakes of magnitude equal to or greater than 7.6. It increases the risk of RIS, while several storage-type hydropower projects are being proposed in Nepal. Seismic activities recorded around the Kulekhani-I reservoir could be a reservoir induced seismicity. However, consistent data of seismic events and reservoir levels during all phases of filling or drawing of water level is missing. This paper reviews the researches on seismic activities caused by reservoirs or tectonic movements, and the need for the study on the mechanism of RIS for the Nepalese context is identified.
尼泊尔水库诱发地震活动性机制综述
全球已记录到90多例水库诱发地震活动。震级在里氏3.0到6.3级之间。水库诱发地震活动性(RIS)可以增加地震活跃带的地震频率,并在地震不活跃带引起冲击。尼泊尔位于地震活跃地带,有6次震级等于或大于7.6级的大地震。它增加了RIS的风险,而尼泊尔正在提出几个储能型水电项目。kulekhani储层周围记录的地震活动可能是储层诱发的地震活动。但是,地震事件与水库蓄水、蓄水各阶段的水位资料缺乏一致性。本文综述了国内外有关储层或构造运动引起的地震活动的研究,指出了尼泊尔地区RIS机制研究的必要性。
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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