Department of Earth System Sciences, Yonsei University, Seoul, Republic of Korea.
Department of Geoinformatics, The University of Seoul, Seoul, Republic of Korea.
Sci Rep. 2017 Jul 14;7(1):5485. doi: 10.1038/s41598-017-06018-0.
We reconstructed the three-dimensional (3D) surface displacement field of the 24 August 2014 M6.0 South Napa earthquake using SAR data from the Italian Space Agency's COSMO-SkyMed and the European Space Agency's Sentinel-1A satellites. Along-track and cross-track displacements produced with conventional SAR interferometry (InSAR) and multiple-aperture SAR interferometry (MAI) techniques were integrated to retrieve the east, north, and up components of surface deformation. The resulting 3D displacement maps clearly delineated the right-lateral shear motion of the fault rupture with a maximum surface displacement of approximately 45 cm along the fault's strike, showing the east and north components of the trace particularly clearly. These maps also suggested a better-constrained model for the South Napa earthquake. We determined a strike of approximately 338° and dip of 85° by applying the Okada dislocation model considering a single patch with a homogeneous slip motion. Using the distributed slip model obtained by a linear solution, we estimated that a peak slip of approximately 1.7 m occurred around 4 km depth from the surface. 3D modelling using the retrieved 3D maps helps clarify the fault's nature and thus characterize its behaviour.
我们利用意大利航天局的 COSMO-SkyMed 和欧洲航天局的 Sentinel-1A 卫星的合成孔径雷达(SAR)数据,重建了 2014 年 8 月 24 日 M6.0 南纳帕地震的三维(3D)地表位移场。利用传统的合成孔径雷达干涉测量(InSAR)和多孔径合成孔径雷达干涉测量(MAI)技术生成的沿轨和跨轨位移被整合,以获取地表变形的东、北和垂直分量。生成的 3D 位移图清晰地描绘了断层破裂的右旋剪切运动,沿断层走向的地表位移最大值约为 45 厘米,显示出断层迹线的东向和北向分量尤为清晰。这些地图还为南纳帕地震提供了一个约束更好的模型。我们通过应用考虑单一均匀滑动运动的 Okada 位错模型,确定了一个大约 338°的走向和 85°的倾角。通过线性解得到的分布式滑动模型,我们估计在距离地表约 4 公里深处,峰值滑动约为 1.7 米。使用所得到的 3D 地图进行的 3D 建模有助于澄清断层的性质,从而描述其行为。