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利用多传感器 SAR 联合反演获取 2014 年 M6.0 南纳帕地震的精确三维形变

Retrieving Precise Three-Dimensional Deformation on the 2014 M6.0 South Napa Earthquake by Joint Inversion of Multi-Sensor SAR.

机构信息

Department of Earth System Sciences, Yonsei University, Seoul, Republic of Korea.

Department of Geoinformatics, The University of Seoul, Seoul, Republic of Korea.

出版信息

Sci Rep. 2017 Jul 14;7(1):5485. doi: 10.1038/s41598-017-06018-0.

Abstract

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.

摘要

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。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/fc84/5511219/c6e0a085829a/41598_2017_6018_Fig1_HTML.jpg

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