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首页> 外文期刊>Geomatics,Natural Hazards & Risk >Himalayan hazard study on the basis of stress and strain state of 1991 Uttarkashi earthquake using Coulomb stress transfer model
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Himalayan hazard study on the basis of stress and strain state of 1991 Uttarkashi earthquake using Coulomb stress transfer model

机译:基于库仑应力传递模型基于1991年Uttarkashi地震的应力和应变状态的喜马拉雅灾害研究

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摘要

Uttarkashi region of Himalaya was struck by a destructive earthquake (M-w = 6.8) on 19 October 1991 with its epicentre located at 30.78 degrees N latitude and 78.77 degrees E longitude.Here, we use Coulomb stress model for the study of this major event. Coulomb 3.1 application is used to generate the earthquake model and develop the stress change maps of the region. The 1991 Uttarkashi earthquake and succeeding earthquakes of M-b > 3.5 are used for the study. One of the motives of this work is to correlate the main shock and the successive minor earthquakes that have occurred in the region. Further, we have studied the 1999 Chamoli earthquake using this model and attempted to relate its occurrence with the Uttarkashi earthquake based on propagation of strain energy.The study of Uttarkashi 1991 earthquake by this method supports the main shock and its controlling effect on the later earthquakes' observations in the nearby region with the view that many zones of such shock can occur in the future. This model is also used to predict the direction of propagation of strain energy, thereby locating the region that will be affected by the future shocks.
机译:喜马拉雅山的Uttarkashi地区于1991年10月19日遭受破坏性地震(M-w = 6.8),震中位于北纬30.78度和东经78.77度,此处我们使用库仑应力模型进行了此次重大事件的研究。库仑3.1应用程序用于生成地震模型并绘制该区域的应力变化图。这项研究使用了1991年的Uttarkashi地震和随后的M-b> 3.5地震。这项工作的目的之一是使该地区发生的主震与连续的小地震相互关联。此外,我们使用该模型对1999年的Chamoli地震进行了研究,并试图通过应变能的传播将其与Uttarkashi地震联系起来。通过这种方法对Uttarkashi 1991年地震的研究支持了主震及其对后期地震的控制作用在附近地区的观察结果表明,未来可能会发生许多此类冲击。该模型还用于预测应变能的传播方向,从而确定将受到未来冲击影响的区域。

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