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- 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。
- 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。
- 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。
- 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。
- Measurements of physical properties indicate that the rutile-bearing eclogite, due to its very high seismic velocity and density, can produce reflections and gravity anomalies. 岩石物性测定表明，金红石榴辉岩的纵波速度极高，会产生明显的反射与重力异常。
- 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。
- Hsieh, S.H., 1972.Subsurface geology and gravity anomalies of the Tainan and Chungchou structure of the coastal plain of southwestern Taiwan, Petrol.Geol.Taiwan, 10, 323-338. 余辉龙、施辉煌、黄春盛、何智刚、曾宝树，1990.;台南县龙船及高雄县坑内、小滚水构造重点地质核查报告，中油内部报告。
- Rao D.B., 1990, Analysis of gravity anomalies of sedimentary basins by an asymmetrical trapezoidal model with quadratic density function, Geophysics, Vol. 55, pp. 226-231. 张忠富，1998，利用数值地形模型从事重力之地形修正研究，国立中央大学地球物理研究所硕士论文，共75页。
- The normalized full gradient and phase of gravity anomalies have been studied by potential field conversion and fast Fourier transform in wave-number domain. 用波数域的位场转换和快速傅立叶变换理论研究重力归一化总梯度和归一化相位;
- Hsieh, S.-H.(1972) Subsurface geology and gravity anomalies of the Tainan and Chungchou structures of the coastal plain of southwestern Taiwan. Petroleum Geology of Taiwan, 10, 323-338. 谢世雄(1972)台湾西南部滨海平原台南及中洲两构造之地下地质与重力异常之研究。台湾石油地质，第10号，第323-338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。
- When gravity survey is conducted in greatly undulate terrain, observed gravity anomaly also includes noise anomalies which are linearly and nonlinearly correlative to land form. 在地形起伏大的地区进行重力测量，所得重力异常中包含了和地形线性相关与非线性相关的干扰异常。
- normalized full gradient of gravity anomalies 重力归一化总梯度
- gravity anomalies forward fitting 重力异常拟合
