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低纬度地区磁法勘探工作体会 被引量:5
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作者 高小光 张勇 《资源环境与工程》 2011年第3期269-271,共3页
位于磁赤道带两侧的低磁纬度区内,在以水平磁化为主的条件下,地下磁性体所产生的△T异常特征与处于中纬度地区的△T异常特征差别较大,提出一种把低纬度地区的磁法测量数据转换成中高纬度地区的转换方法对磁异常进行处理解释,经矿区勘探... 位于磁赤道带两侧的低磁纬度区内,在以水平磁化为主的条件下,地下磁性体所产生的△T异常特征与处于中纬度地区的△T异常特征差别较大,提出一种把低纬度地区的磁法测量数据转换成中高纬度地区的转换方法对磁异常进行处理解释,经矿区勘探对比,效果较好。 展开更多
关键词 低磁纬 △T磁异常特征 二度体异常 磁化方向转换
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Fast forward modeling of gravity anomalies for two-dimensional bodies of arbitrary shape and density distribution
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作者 Chen Xin Chen Long-Wei +1 位作者 Luo Tian-Ya Xiong Bin 《Applied Geophysics》 SCIE CSCD 2020年第5期776-783,902,903,共10页
A fast and high precision spatial domain algorithm is presented for forward modeling of two-dimensional(2D)body gravity anomalies of arbitrary shape and density distribution.The new algorithm takes advantage of the co... A fast and high precision spatial domain algorithm is presented for forward modeling of two-dimensional(2D)body gravity anomalies of arbitrary shape and density distribution.The new algorithm takes advantage of the convolution properties of the expression for 2D gravity anomalies,uses a rectangular cell as a grid subdivision unit,and then 2D bodies with irregular cross-sections are approximated by a combination of 2D bodies with a rectangular cross section.The closed-form expression is used to calculate the gravitational anomalies of the combination of 2D bodies with a rectangular cross section.To improve computing effi ciency,the new algorithm uses a fast algorithm for the implementation of the Toeplitz matrix and vector multiplication.The synthetic 2D models with rectangular and circular cross-sections and constant and variable densities are designed to evaluate the computational accuracy and speed of the new algorithm.The experiment results show that the computation costs less than 6 s for a grid subdivision with 10000×10000 elements.Compared to the traditional forward modeling methods,the proposed method significantly improved computational effi ciency while guaranteeing computational accuracy. 展开更多
关键词 two-dimensional bodies gravity anomalies forward modeling Toeplitz matrix
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