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1·The disturbing gravity is calculated easier than the gravity anomaly.

扰动重力较重力异常更易于重力场计算。

2·For a surveyed gravity anomaly, the combination of some squares is taken as the initial model.

对于一个实测的重力异常，先用若干方格的组合作为初始模型。

3·The forth derivative of gravity anomaly can be obtained by Taylor series expansion of gravity field.

利用重力场的泰勒级数展开式，可求出重力异常的四次导数。

4·There is a new mathod of delimitating faults, that is gravity anomaly linear structure signal mathod.

文中提出了一种划分断裂的方法，即重力异常线性构造信号法。

5·Given a initial model, one can calculate the gravity anomaly caused by a undulate subsurface interface.

在给定密度界面初始模型之后，可以计算出地下某一起伏界面引起的重力异常。

6·The undulation of Mohorovicic discontinuity under JX region only causes the gravity anomaly of 21-42 milligals.

在JX地区，由莫氏界面的起伏只能引起21—42毫伽的重力异常值。

7·According to the data of gravity field in Haljun Basin, the regional distribution of gravity anomaly is obtained.

根据哈喇峻地区区域重力数据资料，给出区域重力异常分布特征。

8·This paper theoretical studies the feasibility of gravity anomaly divided by means of correlation analysis method.

本文从理论上对相关分析法区分重力异常的可行性进行了论述。

9·Conventional methods fail to bring good processing result of gravity anomaly which has undergone terrain correction.

用常规方法对地改后的布格重力异常进行处理效果不佳。

10·The planar gravity anomaly zone reflects geologically active zone, it also easy tof metallic ore deposits formation.

而面状重力异常区则反应了地质活动带，也有利于金属矿床的形成。