2) co-seismic deformation
同震形变
1.
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.
5)在两种成像几何状态下的视线向(LOS)同震形变场。
3) deform in same pace
同步变形
1.
It is showed by experiment that if round compress were large, geogrid would deform in same pace with soil and the value of The equivalent additional compress stress is ea.
通过试验分析表明 ,当周围压力较大时 ,筋土同步变形 ,等效围压值容易确定 ,而周围压力小时 ,筋土不能同步变形 ,等效围压值难以确定 。
4) transformation with the same result
同解变形
5) coseismic displacement
同震形变
1.
The crustal deformation and the coseismic displacement were measured during the 7.
4级地震震前一年的地壳形变和震时同震形变 ,以地震震中为图像中心的 5 0 km× 5 0 km范围内 ,选择了 5景 ERS- 1/ 2数据组成5个像对 ,并在此基础上组成 2个差分像对 ,以分别表示地震前一年形变和同震形变 ,再应用合成孔径雷达干涉测量(In SAR)技术进行处理。
6) co-seismic deformation
同震变形
1.
The co-seismic deformation inversion mode due to seismic fault has been set up considering the earth-stratified structure.
反演结果显示,该反演模式可很好地将断层位错参数反演出来,利用该模式可较好地解决实际地震断层同震变形的反演问题。
2.
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.
顾及地球结构的非均匀性、分层和球体特性,定量研究了球体分层模型、球体均匀模型、半空间均匀模型分别作用于地震断层(走滑断层,逆冲断层)产生的地表同震变形的差异。
补充资料：大坝内部变形观测(见水工建筑物变形观测)
大坝内部变形观测(见水工建筑物变形观测)
daba neibubianxing guanCe大坝内部变形观测见水工建筑物变形观测。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条