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

Author:

Liu Shuang123,Fedi Maurizio2,Hu Xiangyun1,Ou Yang4,Baniamerian Jamaledin25,Zuo Boxin1,Liu Yuegao6,Zhu Rixiang3

Affiliation:

1. Hubei Subsurface Multi-scale Imaging Key Laboratory, Institute of Geophysics and Geomatics, China University of Geosciences, Wuhan, China

2. Department of Earth, Environmental and Resources Science, Naples University of Federico II, Naples, Italy

3. State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, China

4. Institute of Geophysical and Geochemical Exploration, Chinese Academy of Geological Sciences, Langfang, China

5. Department of Earth Sciences, College of Sciences and Advanced Technologies, Graduate University of Advanced Technology, Mahan, Iran

6. Key Laboratory for the Study of Focused Magmatism and Giant Ore Deposits, Ministry of Land and Resources, Xi'an Center of the China Geology Survey, Xi'an, China

Funder

National Natural Sciences Foundation of China

Central Universities, China University of Geosciences

China Postdoctoral Science Foundation

Natural Sciences Foundation of Hubei Province

Publisher

Oxford University Press (OUP)

Subject

Geochemistry and Petrology,Geophysics

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