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1)  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。
2)  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。
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)  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。
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
补充资料:同素异形变化
分子式:
CAS号:

性质:由同种元素组成的结构不同的单质,互称为同素异形体。如氧与臭氧;斜方硫与单斜硫;白磷、红磷与黑磷;石墨,富勒烯碳与金刚石等。互为同素异形体的单质在一定条件下可以互相转化,叫做同素异形变化。如将白磷隔绝空气加热到533K,就转变为红磷;在1215.9MPa压力下,将白磷加热到473K,则能转化为类似石墨的片状结构的黑磷。有些同素异形变化具有重要的实际意义,如高温高压下将石墨变成金刚石等。

说明:补充资料仅用于学习参考,请勿用于其它任何用途。
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