基于Pad有理展开的磁性界面正反演方法

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Bibliographic Details
Published in应用地球物理:英文版 Vol. 13; no. 4; pp. 712 - 720
Main Author 张冲 黄大年 张凯 浦义涛 于平
Format Journal Article
LanguageEnglish
Published 2016
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Bibliography:The magnetic interface forward and inversion method is realized using the Taylor series expansion to linearize the Fourier transform of the exponential function. With a large expansion step and unbounded neighborhood, the Taylor series is not convergent, and therefore, this paper presents the magnetic interface forward and inversion method based on Pade approximation instead of the Taylor series expansion. Compared with the Taylor series, Pade's expansion's convergence is more stable and its approximation more accurate. Model tests show the validity of the magnetic forward modeling and inversion of Pade approximation proposed in the paper, and when this inversion method is applied to the measured data of the Matagami area in Canada, a stable and reasonable distribution of underground interface is obtained.
11-5212/O
Pade approximation, magnetic interface, fand inversion method, Taylor seriesexpansion
Zhang Chong1, Huang Da-Nian1, Zhang Kai2, Pu Yi-Tao3, and Yu Ping1 (1. College of Geo-Exploration Science and Technology, Jilin University, Changchun 130026, China; 2. Mathematics School and Institute, Jilin University, Changchun 130026, China; 3. Bureau of Geophysical Prospecting INC., China National Petroleum Corporation, Korla 841001, China)
ISSN:1672-7975
1993-0658