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Bouguer gravityAnomalies 布格重力异常
Its gravitational field is on a density suddenchange belt of Bouguer anomaly isopleth. 重力场则处于布伽重力异常等值线疏密突变带上。
Therefore, regional geochemical anomalies can be ranked and endogenetic deposits can be forecasted on the basis of Bouguer gravity anomaly data. 因此，应用布格重力异常资料可以推断岩浆岩活动区（带），预测内生矿床，筛选化探异常。
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。
The projection coefficients for Bouguer anomaly are its eigenvalues (square of singular values). 布格异常投影到该正交基上的系数是布格异常矩阵的特征值 (奇异值的平方 ) .
The three dimensional distribution of normalized full gradient of Bouguer gravity is computed by this method. 计算了GH值在地下的三维分布。
Bouguer anomaly is all normal gravity and the magnetic anomaly is almost negative signature in the slop of Qiongdongnan Basin. 琼东南盆地陆坡区布格重力异常值均为正异常,磁异常一般是负异常值。
By using 3-D gravity forward calculation,we obtained the deep gravity anomalies of Tai-wan from its Bouguer anomaly. Its depth corresponds to the lower crust. 经过三维重力正演计算,我们从台湾的布格重力异常中求得了深部重力异常,其深度相当于地壳下层。
Determination of the maximum radius for terrain correction in regional gravity measurement is of significance for improving accuracy of the Bouguer anomaly. 地形改正最大半径的确定,对提高重力布格异常的精度具有重要意义。
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。
Liu, C.-C. and Yen, T.-P. (1975) Bouguer anomaly, surface elevation and crustal thickness in Taiwan. Petroleum Geology of Taiwan, 12, 97-108. 刘珠卿、颜沧波(1975)台湾之布盖重力异常、地形高度及地壳厚度。台湾石油地质，第12号，第97-108页。
Pan, Y.S.(1965)Interpretation and seismic coordination of the Bouguer gravity anomalies obtained in northwestern Taiwan. 经济部中央地质调查所特刊(2000)，第十三号，台湾活动断层概论(二版)。
Pan, Y.S., 1967: Interpretation and Seismic Coordination of the Bouguer Gravity Anomalies over West-Central Taiwan.Petrol.Geol.Taiwan, 5, 99-115. 耿文博(1986)台湾中部竹山及嘉义之地质，经济部地质调查所汇刊，第4号。
Pan, Y. S., 1967: Interpretation and Seismic Coordination of the Bouguer Gravity Anomalies over West-Central Taiwan. Petrol. Geol. Taiwan, 5, 99-115. 何信昌、陈勉铭（2000）台湾地质图台中图幅，经济部中央地质调查所。
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。
Pan, Y.S., 1968.Interpretation and seismic coordination of the Bouguer gravity anomalies over southwestern Taiwan, Petrol.Geol.Taiwan 6, 197-207. 詹新甫与耿文溥，1968.;台湾西南部新第三纪地层及主要地质构造，中国地质学会会刊，第十一号，第45-59页。
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。
What the two ancient lands of Jiangnan and Huaxia caused is a complex magnetic anomaly of equal-axises which corresponds to the gravity Bouguer anomaly in form of "peninsula" . 江南、华夏两古陆所引起的是一复合的等轴磁异常,它与“半鸟”形式的重力布格异常相对应。
The figures of Bouguer anomalies and vertical magnetic anomalies obtained at the scales of 1:1000 000, 1:500 000 and 1:100 000 were processed and the Moho depths were calculated. 本文对天山南麓1:100万、1:50万和1:10万布格重力异常图及相应的垂直磁力异常图进行了处理,并计算了莫霍面深度。
In mountainous area, gravity survey external corrections, including terrain and Bouguer corrections, are the prerequisites for gravity data processing and interpretation. 山区重力勘探中,重力外部校正是重力勘探料处理和解释的前提,其内容包括地形校正、中间校正等。