1) GPS observation velocity
GPS观测速率
2) GPS surveying
GPS观测
1.
In order to study the feasibility of monitoring the change of urban land subsidence by GPS surveying instead of leveling, two periods of GPS observation and leveling were completed respectively in Ningbo city.
研究了用GPS观测取代常规水准测量方法监测城市地面沉降变化的可行性。
2.
It is proved by GPS surveying practice that GPS network structure have remarkable influence on GPS positioning precision.
GPS观测实践证明GPS的网型结构对GPS定位精度具有显著的影响,为了弄清网型结构与GPS定位精度间的关系,在鲁西北平原建立了高精度的专用实验网,专用实验网的三维坐标借助精密电子全站仪和精密水准仪获得。
3.
The feasibility of monitoring the change of city settlement using GPS surveying instead of leveling is studied.
为了研究用GPS观测取代常规的水准测量方法来监测城市沉降变化的可行性,在宁波市建立了有7个点组成的GPS基准网和14个点组成的GPS监测网。
3) GPS observation
GPS观测
1.
The NNW Seismic Belt of Yunnan begins from Zhongdian-Baoshan west of Yunnan, crosses the Eryuan-Heqing fault, Chenghai fault, Honghe fault, Qujiang fault, Lancangjiang fault and Xiaojiang fault, and ends at Xundian and Mile east of Yunnan, on which there are 17 GPS observation stations.
云南北北西地震条带西起中甸、保山,跨越洱源—鹤庆断裂、程海断裂、红河断裂、曲江断裂、澜沧江断裂以及小江断裂等主要活动断裂,止于云南东部的寻甸、弥勒,其上共有17个GPS观测点。
2.
On the basis of GPS observation results of northeastern Tibetan plateau network, we carried out some quantitative experiments on GPS observation optimization of CMONOC project.
中国地壳运动观测网络GPS区域站采用了严格同步环、连续 4天、高站点重复率的观测方案 ,为了优化观测方案 ,以青藏块体东北缘GPS区域网 1999年和 2 0 0 1年观测资料为例 ,对区域GPS观测方案进行了对比试验和分析。
3.
In this paper,we introduced the main content and advance of GPS observation network as well as the summary of 1995-1997 two terms observations.
本文详细介绍了我省GPS观测网络的主要内容与进展 ,以及该观测网络 1 995～1 997二期观测概况 ,观测数据的处理及所得到的结果 ,网内的地壳运动 ,包括网内各部分的应变。
4) GPS stations
GPS观测站
6) GPS measurements
GPS观测
1.
Error analysis of strain rates from GPS measurements based on Monte Carlo method;
基于Monte Carlo方法的由GPS观测计算地应变率的误差分析
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