Downward Continuation and Transformation of Total‐Field Magnetic Anomalies Into Magnetic Gradient Tensors Between Arbitrary Surfaces Using Multilayer Equivalent Sources-Reference-Cited by-同舟云学术

Downward Continuation and Transformation of Total‐Field Magnetic Anomalies Into Magnetic Gradient Tensors Between Arbitrary Surfaces Using Multilayer Equivalent Sources

Published:2020-08-11 Issue:16 Volume:47 Page:
ISSN:0094-8276
Container-title:Geophysical Research Letters
language:en
Short-container-title:Geophys. Res. Lett.

Author:

Zuo Boxin¹^ORCID,Hu Xiangyun²^ORCID,Leão‐Santos Marcelo³^ORCID,Wang Lizhe¹,Cai Yi¹

Affiliation:

1. School of Computer Sciences China University of Geosciences Wuhan China

2. Institute of Geophysics and Geomatics China University of Geosciences Wuhan China

3. Institute of Science and Technology Federal University of Goiás Goiânia Brazil

Funder

National Natural Science Foundation of China

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2020GL088678

Reference28 articles.

1. Estimating source location using normalized magnetic source strength calculated from magnetic gradient tensor data

2. THE EQUIVALENT SOURCE TECHNIQUE

3. A stable downward continuation by using the ISVD method

4. Apparent magnetization mapping in the presence of strong remanent magnetization: The space-domain inversion approach

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