首页> 外文期刊>Geomatics,Natural Hazards & Risk >The 2009 Bhutan and Assam felt earthquakes (M w 6.3 and 5.1) at the Kopili fault in the northeast Himalaya region
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The 2009 Bhutan and Assam felt earthquakes (M w 6.3 and 5.1) at the Kopili fault in the northeast Himalaya region

机译:2009年的不丹和阿萨姆邦在喜马拉雅山东北部的科皮里断裂上感受到了地震(分别为6.3和5.1级)

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Seismotectonics of the two recent earthquakes, one M w 6.3 in the Bhutan Himalaya on 21 September 2009 and the other M w 5.1 in the Assam valley on 19 August 2009, are examined here. The recent seismicity and fault plane solutions of these two felt earthquakes suggest that both the events occurred on the Kopili fault zone, a known active fault zone in the Assam valley, about 300????km long and 50????km wide. The fault zone is transverse to the east?¢????west Himalayan trend, and its intense seismicity indicates that it transgresses into the Himalaya. The geologically mapped curvilinear structure of the Main Central Thrust (MCT) in the Himalaya, where the epicentre of the Bhutan earthquake is located, is possibly caused by the transverse Kopili fault beneath the MCT. This intensely active fault zone may be vulnerable to an impending larger earthquake (M????>????7.0) in the region.
机译:在这里检查了最近两次地震的地震构造,一次地震是2009年9月21日在不丹喜马拉雅山发生的6.3 Mw,另一次地震是在2009年8月19日在阿萨姆邦发生的5.1 MW。这两种毡状地震的最新地震活动和断层平面解表明,这两个事件都发生在阿萨姆邦山谷已知的活动断层带科皮里断层带上,该断层长约300埃·公里,宽50埃·公里。 。断层带横向于东喜马拉雅趋势,其强烈的地震活动表明它进入喜马拉雅山。不丹地震震中所在的喜马拉雅山的主要中央推力(MCT)的地质分布曲线结构,可能是由于MCT下方的横向科皮利断裂所致。这个活跃的断层带可能容易受到该地区即将发生的大地震(M≥7.0> 7.0)的影响。

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