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首页> 外文期刊>Journal of Asian earth sciences >Recent earthquake swarms in Garhwal Himalaya: A precursor to moderate to great earthquakes in the region
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Recent earthquake swarms in Garhwal Himalaya: A precursor to moderate to great earthquakes in the region

机译:Garhwal Himalaya最近的地震群:该地区中度到大地震的先兆

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摘要

Himalayas, one of the most seismically active belts, have been formed due to continent-continent collision and are probable locations for future moderate to great earthquakes. It is of paramount importance to recognize precursory swarm activity considered to be long predictors of main events. Recently two earthquake swarms occurred across Main Central Thrust (MCT) in Garhwal Himalayan region in a time interval of nearly one month. The first swarm of April 2009 had epicentral locations lying north of MCT on hanging wall side, which has shown less seismic activity in recent times, while the second swarm occurred in May 2009 near Copeshwar having epicenters on active seismic zone, located south of MCT. The approximate distance between the two swarms is about 50 km. In present study preparation zone of 100 × 100 km~2 has been demarcated recognizing these swarms as precursors to moderate to great earthquake in the Garhwal Himalaya.
机译:喜马拉雅山是地震活动最活跃的地带之一,是由于大陆与大陆的碰撞而形成的,并且可能是未来中度至大地震的地点。认识到前兆群活动被认为是主要事件的长期预测因素,这一点至关重要。最近,在近一个月的时间间隔内,在加尔瓦尔·喜马拉雅地区的主中央冲断带(MCT)上发生了两次地震。 2009年4月的第一群震中位于MCT悬壁侧以北,最近几次地震活动较少,而第二群发生在2009年5月位于Copeshwar附近,震中位于MCT以南的活跃地震带。两个群之间的大概距离约为50公里。在目前的研究中,已经划定了100×100 km〜2的预备区,认识到这些群是加尔瓦尔喜马拉雅山中度到大地震的先兆。

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