Three-dimensional inversion of magnetic data in the simultaneous presence of significant remanent magnetization and self-demagnetization: example from Daye iron-ore deposit, Hubei province, China
文献类型:期刊论文
作者 | Liu, Shuang1,2,3; Fedi, Maurizio2; Hu, Xiangyun1; Ou, Yang4; Baniamerian, Jamaledin2,5; Zuo, Boxin1; Liu, Yuegao6; Zhu, Rixiang3 |
刊名 | GEOPHYSICAL JOURNAL INTERNATIONAL |
出版日期 | 2018-10-01 |
卷号 | 215期号:1页码:614-634 |
ISSN号 | 0956-540X |
关键词 | Magnetic anomalies modelling and interpretation Rock and mineral magnetism Inverse theory |
DOI | 10.1093/gji/ggy299 |
英文摘要 | Natural remanent magnetization and self-demagnetization on high-susceptibility bodies are two important factors affecting magnetic data inversion. We propose a framework for the inversion and interpretation of magnetic anomalies, in which significant remanent magnetization and self-demagnetization are present simultaneously. The framework is based on the assumptions that the external applied field and internal self-demagnetization field are uniform and the deflection of self-demagnetization in the total magnetization direction is negligible. First, the magnetization vector distributions are obtained from magnetic data by estimating the magnetization direction, then inverting for the magnetization intensity distribution, using the inferred magnetization direction as a constraint. Based on a priori information about the Koenigsberger ratio derived from petrophysical measurements, the direction and intensity of the remanent magnetization are obtained. The self-demagnetization factor is then computed using the finite volume method. Finally, the true-susceptibility distribution is achieved by correcting for the self-demagnetization effect. The method is first applied to synthetic magnetic data produced by a prism-shaped source model that has significant remanent magnetization and high susceptibility. In a case study of the Daye iron-ore deposit, Hubei province, China, the true susceptibility and remanent magnetization are reconstructed. The remanence direction information reveals that local geological activities such as synclines and faults lead to changes in the remanence directions at different local deposits. |
WOS关键词 | NORMALIZED SOURCE STRENGTH ; VECTOR INVERSION ; TOTAL MAGNITUDE ; ERROR ANALYSIS ; DIRECTION ; 3D ; ANOMALIES ; SURFACE ; 2D ; GRAVITY |
资助项目 | National Natural Sciences Foundation of China[41604087] ; National Natural Sciences Foundation of China[41630317] ; National Natural Sciences Foundation of China[41674110] ; Fundamental Research Funds for the Central Universities, China University of Geosciences (Wuhan)[CUGL170407] ; Fundamental Research Funds for the Central Universities, China University of Geosciences (Wuhan)[CUG160609] ; China Postdoctoral Science Foundation[2016M590132] ; Natural Sciences Foundation of Hubei Province[2016CFB122] |
WOS研究方向 | Geochemistry & Geophysics |
语种 | 英语 |
出版者 | OXFORD UNIV PRESS |
WOS记录号 | WOS:000448242600037 |
资助机构 | National Natural Sciences Foundation of China ; National Natural Sciences Foundation of China ; Fundamental Research Funds for the Central Universities, China University of Geosciences (Wuhan) ; Fundamental Research Funds for the Central Universities, China University of Geosciences (Wuhan) ; China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation ; Natural Sciences Foundation of Hubei Province ; Natural Sciences Foundation of Hubei Province ; National Natural Sciences Foundation of China ; National Natural Sciences Foundation of China ; Fundamental Research Funds for the Central Universities, China University of Geosciences (Wuhan) ; Fundamental Research Funds for the Central Universities, China University of Geosciences (Wuhan) ; China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation ; Natural Sciences Foundation of Hubei Province ; Natural Sciences Foundation of Hubei Province ; National Natural Sciences Foundation of China ; National Natural Sciences Foundation of China ; Fundamental Research Funds for the Central Universities, China University of Geosciences (Wuhan) ; Fundamental Research Funds for the Central Universities, China University of Geosciences (Wuhan) ; China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation ; Natural Sciences Foundation of Hubei Province ; Natural Sciences Foundation of Hubei Province ; National Natural Sciences Foundation of China ; National Natural Sciences Foundation of China ; Fundamental Research Funds for the Central Universities, China University of Geosciences (Wuhan) ; Fundamental Research Funds for the Central Universities, China University of Geosciences (Wuhan) ; China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation ; Natural Sciences Foundation of Hubei Province ; Natural Sciences Foundation of Hubei Province |
源URL | [http://ir.iggcas.ac.cn/handle/132A11/89158] |
专题 | 地质与地球物理研究所_岩石圈演化国家重点实验室 |
通讯作者 | Hu, Xiangyun |
作者单位 | 1.China Univ Geosci, Inst Geophys & Geomat, Hubei Subsurface Multiscale Imaging Key Lab, Wuhan, Hubei, Peoples R China 2.Naples Univ Federico II, Dept Earth Environm & Resources Sci, Naples, Italy 3.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing, Peoples R China 4.Chinese Acad Geol Sci, Inst Geophys & Geochem Explorat, Langfang, Peoples R China 5.Grad Univ Adv Technol, Coll Sci & Adv Technol, Dept Earth Sci, Mahan, Iran 6.China Geol Survey, Xian Ctr, Minist Land & Resources, Key Lab Study Focused Magmatism & Giant Ore Depos, Xian, Shaanxi, Peoples R China |
推荐引用方式 GB/T 7714 | Liu, Shuang,Fedi, Maurizio,Hu, Xiangyun,et al. Three-dimensional inversion of magnetic data in the simultaneous presence of significant remanent magnetization and self-demagnetization: example from Daye iron-ore deposit, Hubei province, China[J]. GEOPHYSICAL JOURNAL INTERNATIONAL,2018,215(1):614-634. |
APA | Liu, Shuang.,Fedi, Maurizio.,Hu, Xiangyun.,Ou, Yang.,Baniamerian, Jamaledin.,...&Zhu, Rixiang.(2018).Three-dimensional inversion of magnetic data in the simultaneous presence of significant remanent magnetization and self-demagnetization: example from Daye iron-ore deposit, Hubei province, China.GEOPHYSICAL JOURNAL INTERNATIONAL,215(1),614-634. |
MLA | Liu, Shuang,et al."Three-dimensional inversion of magnetic data in the simultaneous presence of significant remanent magnetization and self-demagnetization: example from Daye iron-ore deposit, Hubei province, China".GEOPHYSICAL JOURNAL INTERNATIONAL 215.1(2018):614-634. |
入库方式: OAI收割
来源:地质与地球物理研究所
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