We processed the ascending and descending pass ASAR radar data that covers the same area using 2-pass D-INSAR technology,and got the co-seismic deformation field in LOS direction of the Bam(Iran) earthquake(Mw6.

Influence of coseismic deformation of the Wenchuan earthquake on the occurrence of earthquakes on active faults in Sichuan-Yunnan region

Taking the InSAR coseismic deformation field as the constraint and adopting the isotropic elastic half-space dislocation model we made the optimum simulation for the geometric form of the fault in which the Gaize Ms 6.

The crustal deformation and the coseismic displacement were measured during the 7.

The co-seismic deformation inversion mode due to seismic fault has been set up considering the earth-stratified structure.

Considering the inhomogeneousness, stratified and spherical characteristic of earth structure, the co-seismic deformation difference among spherical earth layering model, spherical homogeneous model and half-space homogeneous model has been studied in this paper.

Then Zhongba earthquake is selected as an example to obtain the coseismic deformation field with the two-pass differential interferometric processing method.

Based on the analysis of coseismic deformation in the macroscopic epicentral region extracted by Differential Interferometric Synthetic Aperture Radar (D-InSAR), and combined with the seismic activity, focal mechanism solutions of the earthquake and field investigation, the characteristic of coseismic deformation of M S=8.

Mani earthquake was selected as an example to obtain the coseismic deformation field with the three-pass differential interferometric processing method.

Co-seismic deformation waves caused by Indonesia Earthquakes;