首页> 外文会议>2012 IEEE International Geoscience amp; Remote Sensing Symposium. >Three-dimensional surface displacement map of the 2008 Wenchuan earthquake derived from Phase Correlation (PC) sub-pixel offset method and Adaptive Local Kriging (alk) DInSAR data
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Three-dimensional surface displacement map of the 2008 Wenchuan earthquake derived from Phase Correlation (PC) sub-pixel offset method and Adaptive Local Kriging (alk) DInSAR data

机译:基于相位相关(PC)子像素偏移方法和自适应局部Kriging(alk)DInSAR数据的2008年汶川地震三维地表位移图

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Differential Interferometric Synthetic Aperture Radar (DInSAR) is an effective technique to measures the surface displacement caused by strong earthquakes, such as the 2008 Wenchuan earthquake in China. However, in the area subject to the most significant deformation along the Longmenshan fault zone, the coherence between pre- and after- earthquake SAR images is completely lost because of the earthquake induced violent and chaotic destruction on the land surface and consequently, no surface displacement data can be measured. The missing data were recovered using Adaptive Local Kriging (ALK) method to produce a complete Line Of Sight (LOS) displacement map. As a further step to characterize the 3D (three-dimensional) co-seismic deformation, horizontal displacement maps were generated using the Phase Correlation based Image Analysis System (PCIAS), and in combination with the ALK DInSAR data, the vertical displacement map can then be decomposed. Thus, a 3D displacement dataset is accomplished. This dataset shows the thrust and right-lateral strike slip motions along the Longmenshan fault system with two major uplift in Yingxiu and Beichuan areas respectively.
机译:差分干涉合成孔径雷达(DInSAR)是一种有效的技术,可以测量由强地震(例如中国2008年汶川地震)引起的地表位移。但是,在沿龙门山断裂带变形最大的区域,由于地震在地面上引起的剧烈破坏和混乱破坏,震前和震后SAR图像之间的连贯性完全消失了,因此没有地表位移数据可以测量。使用自适应局部Kriging(ALK)方法恢复丢失的数据,以生成完整的视线(LOS)位移图。作为表征3D(三维)同震变形的进一步步骤,使用基于相位相关的图像分析系统(PCIAS)生成了水平位移图,然后结合ALK DInSAR数据,可以得到垂直位移图。分解。因此,完成了3D位移数据集。该数据集显示了沿龙门山断裂系统的逆冲和右旋走滑运动,分别在映秀和北川地区发生了两次大的隆升。

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