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- Ministry of Geology and Mineral Resources. The Bouguer Gravity Anomaly Map of China. 地质矿产部。中国布格重力异常图。
- Using the finite element method for computation of the regional gravity anomaly only need a few data on the boundary. 有限元插值法利用区域边界上的少量数据可计算区域重力异常。
- In dealing with the gravity data of some basin,obtain the residual gravity anomaly applying finite element method. 在某盆地的重力资料处理中;用有限元插值法分离出该区的局部重力异常.
- 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。
- The Bouguer gravity anomaly in Tibetan Plateau is decomposed by wavelet transform and low-pass filter respectively,and applied to the inversion of Moho. 分别采用小波变换和低通滤波对青藏高原地区布格重力异常进行了位场分解和莫霍面反演,并将反演结果与地震资料作比较。
- It is popular to identify the fault and inverse the parameters of the fault with Bouguer gravity anomaly in gravity exploration. 在重力勘探中,一般都要利用布格重力异常来识别断层和反演断层的参数。
- This paper aims to preliminarily discuss the gravity anomaly and the crustal structures from Okinawa Trongh to Mariana Trench (Fig. 1). 本文旨在对冲绳海槽至马里亚纳海沟的重力异常和地壳结构进行初步的研究。
- The Bouguer gravity anomaly in Yinshan-Daqingshan Mountains and Hu-Bao Basin is in "synchronous" agreement with the altitude of the terrain. 根据内蒙古阴山山系及邻近地区的布格重力异常分布特征，发现阴山、大青山山地和呼包盆地地区的布格重力异常分布与地形高程呈“同步型”的特异变化特征。
- In order to interpret the reason of gravity anomaly G8 in Hongqiling orefield, the authors used the choice method which is an inversed method for inversing gravity exploration. 摘要为评价引起红旗岭矿区G8重力异常的原因，采用解重力勘探反演问题的选择法对其进行重新解释评价。
- Lee, T. S., 1949: The topographic reflection of subsurface structures as show by the gravity anomaly in the western plain of Taiwan. Chinese Geophys. Soc. Jour., 1, 205-212. 石再添、张瑞津、杨贵三、许民阳(1985)草屯与车笼埔河阶群的活动层与地形面，中国地理学会会刊，第13期，第1-12页。
- For many years, no matter how the level of gravity explorationmay be, the middle layer and terrain corrections must be done in Bouguer gravity anomaly computation. 多年来，不论重力勘探程度如何，在布格重力异常计算中都必须经过地形改正和中间层改正。
- Isostatic gravity anomaly shows the character of middle - short wavelength, reflects unbalance of crust and upper mantle and dynamical character of substance adjusting. 均衡重力异常显示出中短波长特性,反映的是地壳上地幔物质分布的失衡和物质调整的动力学特征。
- The 1:1000000 regional gravimetric survey deals mainly with physical property and gravity anomaly in the Kangxiwar-Shiquanhe zone on the Qinghai-Xizang Plateau. 摘要提供岩石磁性参数统计表、各地层岩石密度统计表和布格重力异常图，并做初步分析。
- In order to interpret the reason of gravity anomaly G8 in Hongqiling orefield,the authors used the choice method which is an inversed method for inversing gravity exploration. 为评价引起红旗岭矿区G8重力异常的原因,采用解重力勘探反演问题的选择法对其进行重新解释评价。
- After the external correction, the Bouguer gravity anomaly shape may sornetimes change with the elevation, confusing the true anomaly with the false anomaly. 重力测量结果经过外部校正之后，有时布格异常形态会随着高程变化以致形成所谓“山形异常”，使真、假异常混淆。
- Seven large areas (zones) of magmatic activities were detected on the basis of rock density characteristics and Bouguer gravity anomaly data of eastern Inner Mongolia. 摘要依据岩石密度特征，应用布格重力异常资料，在内蒙古东部地区推断7个大型岩浆岩活动区（带）。
- With this method, the role of the gravity data can be brought into full play in oil and gas exploration, and the normal height and gravity anomaly can be jointly determined with very h... 该方法可以充分发挥油气勘探中重力数据的作用,使正常高和重力异常能以很高精度一并地确定出来,如此可满足油气勘探的需要。
- The paper points out, before Tangshan earthquake and during its active period in 1976, a clear change of gravity field oecured in the east part of Beijing network. The ehange has a reverse mark to the gravity anomaly in earthquake foci area. 本文指出,在1976年唐山地震前以及其活动期间,北京测网东部的重力场发生明显的变化,且呈现与震源区重力异常符号相反的变化特征。
- Small scale of mantle convection restricted in asthenosphere diverges in sea basins, converges in Okinawa Trough and Mariana Trough, and it can be generally analogized with isostatic gravity anomaly. 小尺度地幔流主要限于软流圈层内部 ,在各海盆分散 ,而在冲绳海槽和马里亚纳海槽则会聚 ,可与均衡重力异常类比。
- Xisha Trough is arcuate in shape,42Okm long,6-14 km wide and lying at waterdepth of 1500-3400km. The bottom of the trough dips toward east. It is of negative free-air gravity anomaly of-20mgal and positive magnetic anomaly between 50 to 150 nT. 西沙海槽是一条水深1500－3400m、长420km的水槽，新生代沉积厚2－6km。
