地壳运动

dì qiào yùn dòng
  • crustal movement
地壳运动地壳运动
  1. GPS测量研究板块边界的地壳运动和变形

    Studying crustal movement and deformation of plate boundary by GPS Survey

  2. 利用精密水准及GPS数据分析中国东部地壳运动

    Analysis on Eastern China crustal movement by precise leveling and GPS data

  3. GPS揭示的现今地壳运动与地震前兆特征

    Characteristics of current crust movement and seismic precursors revealed by GPS Survey

  4. 青藏高原地壳运动GPS实测结果的定量分析

    Quantitative Analysis of the Crustal Motion of Tiber Plateau Determined by GPS

  5. 中国地壳运动观测网络区域网GPS联测数据的处理

    Data Processing of GPS Campaign of Crustal Movement Observation Network of China

  6. 新疆帕米尔东北侧地区现今地壳运动的GPS监测研究

    Monitoring Present-day Tectonic Deformation by GPS in the Northeast Pamir , Xinjiang

  7. 中国大陆地壳运动的GPS观测及相关动力学研究

    GPS observations for crustal movements in China continent and related geodynamic studies

  8. 利用GPS技术监测中国大陆地壳运动的初步结果

    Preliminary Result of Monitoring Crustal Motion in China by GPS

  9. 福建沿海地壳运动与GPS测量结果初步分析

    Primary analysis of the crustal movement and GPS observation data in Fujian Coast

  10. 天津地区地壳运动观测网络GPS基准站的勘选

    The Survey and Design of the Base Stations in Tianjin Crustal Movement Observation Network

  11. GPS监测地壳运动数据处理

    Data processing for GPS crust movement monitoring network

  12. 用GPS资料分析渭河盆地及邻近地区地壳运动特征

    Analysis of crustal movement feature based on GPS data in Weihe basin and its neighboring region

  13. GPS测量与现今地壳运动;

    GPS survey and crust movement ;

  14. 中国GPS地壳运动监测网的精度分析与评定(1992~1996)

    Precision analysis and estimation of GPS crustal movement monitoring net in China ( 1992 ~ 1996 )

  15. 其中,GPS应用于地壳运动监测和天顶延迟测定均已达到毫米级的精度。

    The accuracy can reach to several millimeters in the crustal movement observation and the determination of zenith delay .

  16. GPS用于区域地壳运动及地震危险区判定的初步研究

    Study on the Horizontal Crust Movement and Emphasized Seismic Surveillance Areas of North China by Using of GPS Data

  17. GPS测定的运动速率和方向与由地质和地震资料推断青藏块体的现代地壳运动特征基本一致。

    The velocity and orientation determined by GPS are rather consistent with that obtained by geologic and seismic data .

  18. 通过分析中国大陆地壳运动GPS速度场得到现今构造应变率场。

    We obtain contemporary tectonic strain rates of Chinese continent from analyzing crustal motion inferred from GPS velocity field .

  19. GPS监测获得高原北部地壳运动速率,发现两个涡旋构造;

    GPS monitoring of the rate of crustal movement in the northern part of the plateau shows two whirl structures ;

  20. 甘肃天祝现代地壳运动GPS监测网的建立与第一期观测初步结果

    Establishment of GPS network for monitoring recent crustal motion in Tianzhu area , gansu and initial results of the first observation

  21. 全球定位系统GPS是利用监测地壳运动进行地震预测的新手段。

    The Global Positioning System ( GPS ) is used to monitor crustal movement which is the new method for earthquake prediction .

  22. 建立了同时顾及坐标框架系统参数和地壳运动参数的GPS网联合平差模型。

    The adjustment model for combined GPS networks considering systematical parameters for the coordinates frames and parameters for the crustal movement is established .

  23. 青藏高原地壳运动与形变的GPS研究&第1期观测的精密星历解

    Study on the Crust Movement & Deformation in QH-XZ Plateau via GPS Observation ── the Solution Using Precies Ephemeris for the First term Observation

  24. 根据中国大陆最新的GPS观测结果研究中国大陆的现今地壳运动和形变特征及其与地震活动的关系。

    In addition , the characteristics of crustal movement and deformation in China are studied on the basis of GPS survey carried out in recent years .

  25. 宁夏地区GPS监测网建设、近期地壳运动特征及应力场与地震活动关系初探

    Establishment of the GPS Monitoring Network in the Middle Part of Ningxia and Preliminary Study of Relationship between the Crustal Deformation and the Stress Field and Seismicity

  26. 并完成了全国GPS一、二级网与中国地壳运动观测网络联测的技术设计方案。

    The technical design scheme of combined observations on the first order and second order 01 networks and the crustal movement observation network of China has been performed .

  27. VLBI和GPS是两种完全不同的观测技术,它们测得的地壳运动有可能是完全不同的情况。

    GPS and VLBI is complete different observed technology , so the crustal motion deduced from them may be absolute unlikeness .

  28. 结果表明,利用GPS定位系统在北极地区进行大规模范围内、高精度监测地壳运动和环境动态变化是完全可行的。

    The results show that it is feasible in Arctic to utilize GPS to monitor crust movement and dynamic variations of environment with high accuracy within large scale range .

  29. 对2000年7月14日大耀斑爆发前后一周时间内,中国地壳运动观测网络的GPS资料进行了分析。

    The GPS data from Crustal Movement Observation Network of China ( CMONOC ) in a week time before and after the flare burst on July 14,2000 are analyzed .

  30. 采用球面非连续变形分析(DDA)模型,以GPS观测得到的速度值为约束,拟合出了中国大陆现今地壳运动的速度场。

    Then the China Continent velocity field is established , by using the spherical discontinuous deformation analysis ( DDA ) model .