| 1. | Determination of fuxin quasi - geoid without gravity data
无重力数据情况下阜新似大地水准面的确定 |
| 2. | Application of joint inversion of magnetotelluric , seismic and gravity data in xuwen area
地震与重力资料综合反演在徐闻地区的应用 |
| 3. | With the size and gravity data all set we can finally create the simulator object
与大小和重力数据一起设置让我们能创建最终的模拟器对象。 |
| 4. | Determination of linear and periodic error parameters for the scale value of lcr gravimeters by observed gravity data
重力仪的线性格值和周期误差参数 |
| 5. | Analysis and tectonic interpretation to the horizontal - gradient map calculated from bouguer gravity data in the china mainland
中国布格重力异常水平梯度图的判读和构造解释 |
| 6. | Typical examples for triple decomposition of local anomalies are given by using gravity data obtained from chinese continental scientific drilling site
中国大陆科学钻探场地的重力异常分解给出局部异常分解的典型例子。 |
| 7. | Discrepancies between measurements on different tracks may exist at the intersection because airborne gravity data are unavoidably affected by different kinds of error source
由于受到各种误差源的干扰和影响，造成了交叉点上重力观测值不相同，即存在交叉点重力观测值不符值。 |
| 8. | Based on the analyzing of the dss ' s basic theory of tomography , an inversion scheme that can be described as the combination of the finite - difference inversion and ray inversion using traveltime , amplitude and gravity data is proposed
在分析深地震测深剖面层析成像基本理论的基础上提出了利用走时、振幅和重力数据，通过有限差分反演和射线反演方法对地壳上地幔结构进行层析成像的研究思路。 |
| 9. | The third chapter of this paper explored the method of acquiring amplitude - ratio , and also the significance of the amplitude and gravity data for the probing of the crust and upper mantle ' s structure is investigated . thus the framework of inversion adopted by this paper is formed
本文第三章研究了相对振幅比的获取方法，探讨了利用振幅和重力资料模拟来约束地壳速度结构的有效性，从而形成本文层析成像工作的总体结构。 |
| 10. | The temporal , spatial and frequency - field characteristics are discussed . the validity of the corresponding empiric formula is analyzed and the atmospheric effects and correction method are investigated in the data analysis of the ground - based observations . the atmospheric effects on the gravity observations are analyzed and detected using the gravity data recorded with the superconducting gravimeters at the global geodynamic project ( ggp ) stations
利用实测地面气温、气压资料获得大气负荷效应时间序列的数值结果，研究大气影响的时间、空间和频率特征，分析经验公式的有效性，研究地面观测和数据分析大气影响和改正的方案；利用ggp台站超导重力观测资料，分析检验大气重力影响；分析igs台站大气位移改正的可能性 |
