首页> 外文会议>Dragon 3 Final Results amp; Dragon 4 Kick-Off Symposium >DEVELOPMENT AND IMPLEMENTATION FOR CALCULATION MODEL OF MEASURING CO-SEISMIC DEFORMATION FIELD BY USING ASCENDING AND DESCENDING ORBIT SAR DATA
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DEVELOPMENT AND IMPLEMENTATION FOR CALCULATION MODEL OF MEASURING CO-SEISMIC DEFORMATION FIELD BY USING ASCENDING AND DESCENDING ORBIT SAR DATA

机译:利用升,降轨道SAR数据测量同震形变场计算模型的开发与实现

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摘要

Interferometry Synthetic Aperture Radarrn(InSAR)can only measure one component of thernsurface deformation in the satellite's line of sightrn(LOS) instead of that in vertical and horizontalrndirections, i.e. LOS Amphibious. In view of thisrnproblem, we analyzed and summarized somernmethods that can measure the three-dimensionalrndeformation of ground surface by using D-InSAR,rndeveloped the calculation model of measuring thernthreedimensional co-seismic deformation filed byrnusing the ascending and descending orbit SAR data.rnThe Formula of left-looking (both ascending andrndescending orbit data), right-looking (bothrnascending and descending orbit data) and generalrnexpression were proposed. The model was appliedrnon L'Aquila earthquake, and the results reveal thatrnthe earthquake has caused displacement in bothrnvertical and horizontal directions, and thernearthquake made the area down lift 16.8cm alongrnthe vertical direction. The characters of the surfacernreflected by the results are very consistent with therngeological exploration.
机译:干涉测量法合成孔径雷达(InSAR)只能测量卫星视线(LOS)中表面变形的一个分量,而不能测量垂直和水平方向上的视差,即LOS两栖的。针对这一问题,我们分析和总结了一些可以利用D-InSAR来测量地表三维变形的方法,开发了利用上升和下降轨道SAR数据来测量三维同震变形的计算模型。提出了向左看(上升和下降轨道数据),向右看(上升和下降轨道数据)以及一般表达式。该模型应用于拉奎拉地震,结果表明该地震在垂直和水平方向上都引起了位移,并且地震使该区域沿垂直方向下降了16.8cm。结果反映出的地表特征与地质勘探非常吻合。

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  • 会议地点 Wuhan(CN)
  • 作者单位

    Institute of Engineering Mechanics, China Earthquake Administration, Harbin 150090,China,Tengfei_Xue@126.com Key Laboratory of Crustal Dynamics, Insitute of Crustal Dynamics, China Earthquake Administration,Beijing 100085, China;

    College of Resource, Environment and Tourism, Capital Normal University, Beijing 100048, China;

    Key Laboratory of Crustal Dynamics, Insitute of Crustal Dynamics, China Earthquake Administration,Beijing 100085, China;

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  • 正文语种 eng
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