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Numerical Modeling of the Stress-Strain State and Results of GPS Monitoring of the Epicentral Area of the August 24, 2014 Earthquake (Napa, California, USA)

机译:2014年8月24日地震(美国加利福尼亚纳帕)震中地区的应力应变状态数值模拟和GPS监测结果

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This paper reports the results of numerical modeling of the stress-strain state of the epicentral area before and after the August 24, 2014 earthquake in Napa, California, USA, compared to calculated data obtained in instrumental studies in the dilatation areas based on GPS observation results. Numerical modeling has made it possible to calculate the stress-strain state of the epicentral area affected by the tectonic fault system. GPS observation data on the epicentral area of the earthquake and the results of numerical modeling of the stress-strain state before and after the considered earthquake have been analyzed. A trend toward localization of earthquake epicenters in the region of high stress intensity concentration has been confirmed. It has been proved that aftershock development is due to the drop in stress caused by a new fracture and that the aftershock cluster that occurred was localized in the area of decreased stress intensity.
机译:本文报告了2014年8月24日美国加利福尼亚纳帕地震前后震中区域应力应变状态的数值模拟结果,并与基于GPS观测的扩张地区仪器研究获得的计算数据进行了比较结果。数值建模使得计算受构造断裂系统影响的震中区域的应力应变状态成为可能。分析了地震震中地区的GPS观测数据以及考虑地震前后的应力-应变状态的数值模拟结果。已经确认了在高应力强度集中区域中地震震中局部化的趋势。业已证明,余震的产生是由于新的裂缝引起的应力下降所致,而发生的余震簇位于应力强度降低的区域。

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