1) secular crustal deformation
地壳缓慢变形
2) Slowly varying topography
缓慢变化地形
3) slowly changing topography
缓变地形
1.
KdV equation with a forcing term for the evolution of the amplitude of Rossby waves along a slowly changing topography;
缓变地形下Rossby波振幅演变满足的带有强迫项的KdV方程
4) crust deformation
地壳形变
1.
The space measurement and control stations are distributed in the different plates all over the world,and the site coordinates must be changed according to crust deformation.
航天测控站分布在全球不同的板块,其站址坐标随地壳形变而发生变化。
2.
It is shown that Dali area will be one of the most hazard zone of earthquake of Yunnan Province in the future ten years, based on the analyses of tendency variation of precursor factors of geomagnetic, gravity fields, crust deformation and ground water in the area for many years.
通过对大理地区多年来地磁场、重力场、地壳形变和地下水等地震前兆因素变化趋势的分析，指出大理地区是云南省未来１０年内发生强震危险性最大的区域之一。
3.
According to our research in the southern Tibet, based on the summary and analysis of researching results domestics and overseas, this thesis systematically study the problem of crust deformation of south Tibetan Plateau with geology tectonic, deformation model, GPS data process and forward and inversion of crust deformation.
本文以青藏高原南部为研究背景，在总结分析国内外研究成果的基础上，从地质构造、形变分析模型、GPS数据处理以及地壳形变正反演分析等多方面对南部青藏地壳形变运动进行系统的分析研究，得到了一些有益的结论和认识。
5) crustal deformation
地壳形变
1.
Characteristics of present-day crustal deformation and seismicity in western China;
中国西部现今地壳形变与地震活动特征
2.
Floating velocity calculation in GPS crustal deformation monitoring;
GPS监测地壳形变漂移速度的计算
3.
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) crustal deformation
地壳变形
1.
In order to integrally interpret the modern geodetic data, on the basis of available works,we put forward the basic concept of the coupling movement between the crustal deformation and density change, analyze the theory of coupling movement, and derive a general strict formula of time-varying grav- ity caused by the coupling movement.
为整体解释现代大地测量数据,提出了地壳变形与密度变化耦合运动的基本思想;分析了地壳变形与密度变化耦合运动的基本理论;导出了由地壳形变与密度变化耦合运动引起的重力时间变化一般严格公式。
2.
Moho depth distribution and crustal deformation pattern between different sub-blocks in Sichuan-Yunnan region are presented here based on the studies of the gravity field characteristics.
滇西地区布格重力一阶导数与现今地壳变形格局总体一致,主体构造方向为北北西-近南北向,代表了“新”构造主体构造线的方向;上延至4 5km后,主体构造上转变为以近东西向为
3.
Active tectonics is the important manifestation of the present crustal deformation.
活动构造是现今大陆地壳变形的重要反映。
补充资料：缓慢
不迅速；慢：行动～。
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