摘要
为了更好地研究地壳形变细节和运动机理,需要获取地壳精确三维形变场的方法。本文首先介绍重构三维形变场理论的发展历程,综述了目前几种主流的重构三维形变场的方法,包括:基于升、降轨SAR干涉对测量和方位向形变测量,构建模型获取三维形变场;联合GPS和DInSAR测量的形变值,构建模型解算三维形变场;联合多个视角的视线向形变观测结果,构建线性模型解算三维形变场。每种方法都有各自的特点、也有其特定的使用范围,本文对这些方法以及它们的特点进行总结,在此基础上对重构三维形变场理论的发展进行展望。
In order to better study the details and movement mechanism of crustal deformation,some scholars have actively explored the method of obtaining the accurate three-dimensional deformation field of the crust.In this article,we firstly analyze the necessity of reconstructing 3 D deformation field,and review the development history of the theory about reconstruction of threedimensional deformation field.After introducing the DInSAR technology,several main methods of reconstruction of 3 D deformation fields are described,including the acquisition of three-dimensional deformation field based on the measurement relying on the rise and descending SAR interferometry and azimuth deformation measurement,combining GPS and the deformation values of DInSAR measurements to construct a three-dimensional shape change field,combining observation results about the line of sight alignment with multiple angles of view to construct a three-dimensional shape change field.Each method has its own characteristics and its specific scope of use,this article is about the methods and their characteristics,then on the basis of this,shows the future development of the theoryof 3 D deformation fieldreconstruction.
作者
纪润池
张景发
申旭辉
李永生
Ji Runchi;Zhang Jingfa;Shen Xuhui;Li Yongsheng(Institute of Crustal Dynamics,CEA,Beijing,100085,China)
出处
《地壳构造与地壳应力文集》
2018年第1期136-149,共14页
Bulletin of the Institute of Crustal Dynamics
基金
中央级公益性科研院所基本科研业务重点专项(ZDJ2017-29)
国家自然科学基金(41704051)
民用航天项目(D010102)