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首页> 外文期刊>Geophysical Research Letters >Displacement field and fault model for the September 7, 1999 Athens earthquake inferred from ERS2 satellite radar interferometry
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Displacement field and fault model for the September 7, 1999 Athens earthquake inferred from ERS2 satellite radar interferometry

机译:根据ERS2卫星雷达干涉仪推断1999年9月7日雅典地震的位移场和断层模型。

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On September 7, 1999, a moderate (M-n = 5.9) normal faulting earthquake occurred in the northwest of Athens (Hellas) causing heavy damages and casualties. Using interferometric combinations of ERS2 SAR images, we analyzed the coseismic deformation field. Two fringes are observed south of the Fill mountain, up to the coastline of the Elefsis gulf. They correspond to 56 mm increase in slant range. Modeling the earthquake as a dislocation in an elastic half-space, we inverted the interferometric data to assess the fault location and geometry and the amplitude of the coseismic slip. The model suggests similar to 300 mm slip on an 18 km long blind fault composed of two pieces. The intersection of the fault plane with the Earth surface is located in the Fill mountain with a similar to N120 degrees orientation. [References: 14]
机译:1999年9月7日,雅典(Hellas)西北发生了中等(M-n = 5.9)正常断层地震,造成了严重的人员伤亡。使用ERS2 SAR图像的干涉组合,我们分析了同震形变场。在Fill山以南,直至Elefsis海湾的海岸线,都观察到两个边缘。它们对应于倾斜范围增加了56 mm。将地震建模为弹性半空间中的位错,我们反转了干涉数据,以评估断层的位置和几何形状以及同震滑动的幅度。该模型表明,在由两块组成的18 km长的盲断层上,滑移量约为300 mm。断层平面与地球表面的交点位于Fill山中,方向类似于N120度。 [参考:14]

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