崩错-东巧共轭断裂带是青藏高原中部一系列共轭走滑断裂系的重要组成部分，目前对该共轭走滑断裂带运动学调节机制的研究相对较少。因此本申请选择崩错-东巧共轭走滑断裂系为研究对象，应用最新的Sentinel-1 IW 宽幅SAR数据，通过构建宽幅InSAR时序分析流程框架和误差校正算法，旨在提高宽幅InSAR对微小形变信息的提取精度。方法包括：1)以满秩矩阵原则提高相干点密度和信号稳定性; 2)利用小基线网络法和高分辨ECMWF大气数据辅助下校正宽幅干涉图中大气延迟误差; 3)闭合残差方法校正离散点相位解缠误差；4)利用联合解算模型分离长波长断裂形变信号与轨道误差信号。最终获取整个崩错-东巧共轭走滑断裂带的构造形变特征，并联合GPS资料分析崩错-东巧共轭走滑断裂系整体运动机制，研究该共轭走滑断裂系在时间和空间上的应变调节问题，有助于理解青藏高原中部发育的一系列共轭走滑断裂系的运动特征。

Research on the slip kinematics of the Bengco-Dongqiao conjugate strike-slip fault system, located in the central Tibetan Plateau, is important for understanding the outward growth of the Tibet. There is rare study focused on this before. We plan to apply and develop a technology named Wide-scan Sententinel-1 IW to work on this question. We try to analyze an overall deformation pattern for this conjugate strike-slip fault system. Besides, a set of the Sentinel-1 Interferometric Wide SAR data will be processed to achieve their Wide-scan InSAR time series results and also produce the error correction algorithm. The followings are our works: (1) We will use the principle of full rank matrix to improve the density and the stability of the coherent points, (2) The network method and high resolution ECMWF data assisted for atmospheric delay error correction, (3) the closed-phase loop method for correcting unwrapping phase error and, (4) The joint model was used to separate the long wave signal of fault deformation from orbit error. Finally, combined with GPS data, we will analysis the whole motion characteristics of conjugate strike-slip faults，investigate the strain accumulation of tectonic deformation in time and space. It is helpful to understand the characteristics of a series of conjugate strike slip faults developed in the middle part of the Qinghai Tibet Plateau