1、

Harmonic analysis of the gravity tidal data observed at the Shanghai station from April to august, 1978

上海台重力固体潮观测结果(1978年4月&8月)的调和分析

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2、

By using 11 global ocean tide models and tidal gauge data obtained in the East China Sea and South China Sea, the influence of the ocean loading on gravity field in China and its neighbor area is calculated in this paper.

利用11个全球海潮模型和中国东海及南海近海潮汐资料,计算了海潮负荷对中国及邻区重力场的影响,进而讨论了用近海潮汐资料修正全球海潮模型对负荷结果的影响。

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3、

Analysis of gravity tide data and determination of fundamental tide factors in the western Yunnan

滇西地区重力潮汐观测资料的分析处理及潮汐基准参数的确定

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4、

In order to use the gravity tide data for earthquake prediction some suggestions have been made at the end.

最后,就利用重力固体潮资料予报地震的观测方法提出了几点建议。

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5、

In this paper, it is pointed out theoretically that the ground surface tilt is not observed by only tiltmeter, but must be determined by both tilt and gravity earth tide data.

本文从理论上阐述了单靠倾斜仪不能监测地面倾斜,必须联合倾斜和重力固体潮资料才能测量地面倾斜。

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6、

In this paper, examples are given to show how to calculate from navigation positioning data the required variables and corresponding RMS errors which are used to work out Eotvos corrections, and the geographic coordinates of every gravity station.

文中举例说明如何根据导航定位数据求出所需的用于计算厄缶校正的各个变量和相应的均方误差,以及各个重力测点的地理位置。

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7、

The application of glide correlation analysis to the interpretation of gravity and magnetic data

滑动相关分析在重磁资料解释中的应用

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8、

Calibration for CHAMP Accelerometry Data Based on Known Earth Gravity Field Model

利用现有重力场模型求定CHAMP卫星加速度计修正参数

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9、

Recovery of earth gravity field with CHAMP data of orbit and acceleration

应用CHAMP卫星轨道和加速度数据恢复地球重力场

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10、

Earth's Gravity Field Recovered from CHAMP Science Orbit and Accelerometer Data

利用CHAMP科学轨道数据和星载加速度计数据反演地球重力场

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11、

Application surfer in visualization of earth gravity field data

Surfer在地球重力场数据可视化中的应用

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12、

The design of a gravity and magnetic data processing system

重磁数据处理系统设计

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13、

After processing gravity and aeromagnetic data, we infer that the Haiyang Island and Liugong Island uplifts are connected by two smaller uplifts in NW direction, and these two smaller uplifts divide the North Yellow Sea basin into three parts.

通过重磁数据处理解释推测认为:两条NW向的次级隆起将海洋岛隆起与刘公岛隆起连接起来,同时将北黄海盆地分成3部分;

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14、

Under the condition of reliable GPS/ level data, boundary restriction to gravitational height anomaly model is made, which aims at weakening the system errors existing in the transform between gravity system and height system, achieving the system transform, improving precision of ultimate model.

在确保GPS/水准点成果可靠的前提下,用其对重力法计算所得的高程异常模型进行框架约束,以削弱重力系统与高程和坐标系统间的系统差,实现系统转换,提高最终模型的精度。

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15、

Gravity and magnetic data processing and plotting FORTRAN program tool kit

重、磁数据处理和图象显示FORTRAN程序库

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16、

comparing the gravity anomalies derived from igggrace01s ( 72 degree) with nima gravity anomalies data ( 2.5 °× 2.5 °), the standard deviation is 4.8 mgal in china land region.

对于中国大陆,比较IGGGRACE01S模型(前72阶)计算的重力异常和NIMA重力异常数据(2.5°×2.5°网格),两者之间的标准偏差为4.8mGal。

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17、

Processing and interpretation of gravity anomaly data in Dagang-west Bohai area

大港&渤海西部地区重力异常数据的处理和解释

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18、
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