1) 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。
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) 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。
4) coseismic deformation
同震形变
1.
Influence of coseismic deformation of the Wenchuan earthquake on the occurrence of earthquakes on active faults in Sichuan-Yunnan region
汶川地震同震形变场对川滇地区主要活动断裂地震发生趋势的影响
2.
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.
以InSAR同震形变场为约束,采用各向同性弹性半空间位错模型,利用试错法对2008年西藏改则县扎西错Ms6。
5) coseismic deformation
同震形变场
1.
Then Zhongba earthquake is selected as an example to obtain the coseismic deformation field with the two-pass differential interferometric processing method.
本文简要介绍了InSAR及其差分技术的基本原理,并以仲巴地震为例,采用已知DEM的二路差分法获取了仲巴地震的同震形变场。
2.
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.
利用差分干涉雷达测量技术获取的宏观震中区的同震形变场 ,结合对地震活动性、震源机制、野外考察等资料分析 ,对昆仑山口西 8。
3.
Mani earthquake was selected as an example to obtain the coseismic deformation field with the three-pass differential interferometric processing method.
以西藏玛尼地区为例,通过三通差分干涉处理,获取了玛尼地震同震形变场。
6) Co-seismic deformation waves
同震形变波
1.
Co-seismic deformation waves caused by Indonesia Earthquakes;
印尼强地震引起的同震形变波
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