基于小波正则化方法的三维磁数据反演

Q4 Earth and Planetary Sciences
M. Abedi, H. Siahkoohi, A. Gholami, G. Norouzi
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引用次数: 8

摘要

本文在反演算法中引入稀疏性约束,研究磁化率模型的三维恢复问题。为此,勘探区域被划分为大量的矩形棱镜,在一个网格中具有未知的磁化率。采用带两个稀疏度函数的Tikhonov代价函数恢复模型参数的光滑部分和尖锐边界。预先选择的基即小波可以恢复磁化率分布的光滑行为区域,而哈尔或有限差分(FD)域产生具有粗糙边界的解。因此,选择一个正则化函数作为模拟磁异常的候选函数,该函数可以利用小波和Haar/FD算子在表示三维磁化率分布方面的优势。同时考虑了控制两种稀疏化算子权值的最优小波和参数β。该算法假设不存在剩余磁化,并观察到磁强计数据仅代表感应磁化效应。将该方法应用于含噪声的合成数据反演,验证了该方法在磁资料三维反演中的适用性。在取得满意结果的基础上,以伊朗Kerman地区某斑岩铜矿地面磁异常测量为例,对Chun矿床进行了三维反演。所建模型的低磁化率与已知的铜矿成矿位置相吻合。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
3D Inversion of Magnetic Data through Wavelet based Regularization Method
This study deals with the 3D recovering of magnetic susceptibility model by incorporating the sparsity-based constraints in the inversion algorithm. For this purpose, the area under prospect was divided into a large number of rectangular prisms in a mesh with unknown susceptibilities. Tikhonov cost functions with two sparsity functions were used to recover the smooth parts as well as the sharp boundaries of model parameters. A pre-selected basis namely wavelet can recover the region of smooth behaviour of susceptibility distribution while Haar or finite-difference (FD) domains yield a solution with rough boundaries. Therefore, a regularizer function which can benefit from the advantages of both wavelets and Haar/FD operators in representation of the 3D magnetic susceptibility distributionwas chosen as a candidate for modeling magnetic anomalies. The optimum wavelet and parameter β which controls the weight of the two sparsifying operators were also considered. The algorithm assumed that there was no remanent magnetization and observed that magnetometry data represent only induced magnetization effect. The proposed approach is applied to a noise-corrupted synthetic data in order to demonstrate its suitability for 3D inversion of magnetic data. On obtaining satisfactory results, a case study pertaining to the ground based measurement of magnetic anomaly over a porphyry-Cu deposit located in Kerman pr of Iran ow Chun deposit was presented to be 3D inverted. The low susceptibility in the constructed model coincides with the known location of copper ore mineralization.
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来源期刊
International Journal of Mining and Geo-Engineering
International Journal of Mining and Geo-Engineering Earth and Planetary Sciences-Geotechnical Engineering and Engineering Geology
CiteScore
0.80
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0.00%
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审稿时长
12 weeks
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