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- 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。
- 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。
- Pan, Y.-S.(1968) Interpretation and seismic coordination of the Bouguer gravity anomalies obtained in southwestern Taiwan. Petroleum Geology of Taiwan, 6, 197-207. 潘玉生(1968)台湾西南部诸重力异常与震测结果之研究。台湾石油地质，第6号,，第197-207页。
- Pan, Y.-S.(1967) Interpretation and seismic coordination of the Bouguer gravity anomalies over west-central Taiwan. Petroleum Geology of Taiwan, 5, 99-115. 潘玉生(1967)台湾中西部诸重力异常与震测结果之比较研究。台湾石油地质，第5号，第99-115页。
- Pan, Y.-S.(1965) Interpretation and seismic coordination of the Bouguer gravity anomalies obtained in northwestern Taiwan. Petroleum Geology of Taiwan, 4, 287-301. 潘玉生(1965)台湾西北部诸重力异常与震测结果之比较研究。台湾石油地质，第4号，第287-301页。
- The section density model wasessablished with the help of variable density horizontal trapezoid body,ac th6 calculated theoretical anomalies are coincideal with the measured Bouguer gravity anomalies. 根据剖面密度模型，可以合理地解释布格重力异常。
- 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 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。
- 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。
- 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。
- 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）。
- Bouguer gravity anomalies 布格重力异常
- 1. 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。收藏指正
- 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。
