| 1. | It is often impossible to differentiate between structure and density contrast in determining the source of a gravity anomaly .
在确定重力异常源时，不可能在构造与密度差之间作出抉择。 |
| 2. | These gravity anomalies correspond to positive aeromagnetic anomalies and are interpreted as being due to buried volcanic or intrusive rock .
这种重力异常和航磁异常相符，其原因可能是有隐伏的火山岩和侵入岩。 |
| 3. | Observed gravity anomaly
观测重力异常 |
| 4. | Wavelet analysis results of gravity anomalies and its geological significance in hefei basin
合肥盆地重力异常特征及其地质意义 |
| 5. | Gravity anomaly chart
重力异常图 |
| 6. | Study of faulted structure using the normalized full gradient of gravity anomaly and its phase
利用重力归一化总梯度及相位法研究断裂构造 |
| 7. | A regularization algorithm of the integral equation for an gravity anomaly inverse problem of faultage effect
断层模型重力异常反演的正则化算法 |
| 8. | Over - determined model for computing gravity anomaly based on regularization solution of discrete integration eguation
基于积分方程正则化的重力异常超定问题解法 |
| 9. | The high gradients of bouguer gravity anomalies and seismotectonics of moderate earthquakes in jianghuai region , china
江淮地区布格重力异常与中强地震发生的构造环境分析 |
| 10. | The paper proposed the characteristics and inversion method of gravity anomalies spectrum using cosine transform
摘要提出利用余弦变换，研究规则体重力异常谱特征及反演方法。 |
