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Coseismic Deformations of the Earth's Surface in Sakhalin Related to the August 2, 2007, M-w=6.2 Nevelsk Earthquake

机译:与2007年8月2日M-w = 6.2 Nevelsk地震有关的萨哈林岛地球表面的同震形变

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The satellite radiointerferometry data revealed deformations of the coastal part of Sakhalin Island caused by the earthquake with M-w = 6.2 that occurred in the Tatar Strait near Nevelsk. Based on the joint analysis of the satellite and seismological data, dislocation models were contrived for the main shock and its strong aftershocks with the western dip of the fault planes. This made it possible to determine the source mechanisms and the geometrical parameters of the seismic ruptures and to calculate the coseismic vertical and horizontal displacements. In contrast to the one-dimensional model of the insular land displacements determined from the satellite radiointerferometry measurements, this provided a three-dimensional model of the surface deformations for the epicentral zone.
机译:卫星无线电干涉仪数据显示,内维尔斯克附近塔塔尔海峡发生的M-w = 6.2地震引起的萨哈林岛沿海地区变形。在对卫星资料和地震资料进行联合分析的基础上,建立了以断层平面西倾角为主震及其强余震的位错模型。这使得确定地震破裂的震源机制和几何参数以及计算同震垂直和水平位移成为可能。与通过卫星无线电干涉测量法确定的岛屿陆地位移的一维模型相反,这为震中区提供了表面变形的三维模型。

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