Progressive Dissolution of Titanomagnetite in High‐Temperature Hydrothermal Vents Dramatically Reduces Magnetization of Basaltic Ocean Crust-Reference-Cited by-同舟云学术

Progressive Dissolution of Titanomagnetite in High‐Temperature Hydrothermal Vents Dramatically Reduces Magnetization of Basaltic Ocean Crust

Published:2020-04-15 Issue:8 Volume:47 Page:
ISSN:0094-8276
Container-title:Geophysical Research Letters
language:en
Short-container-title:Geophys. Res. Lett.

Author:

Wang Shishun¹^ORCID,Chang Liao¹²^ORCID,Wu Tao³,Tao Chunhui³⁴^ORCID

Affiliation:

1. Laboratory of Orogenic Belts and Crustal Evolution, School of Earth and Space Sciences Peking University Beijing China

2. Laboratory for Marine Geology Qingdao National Laboratory for Marine Science and Technology Qingdao China

3. Key Laboratory of Submarine Geosciences, Second Institute of Oceanography Ministry of Natural Resources Hangzhou China

4. School of Oceanography Shanghai Jiao Tong University Shanghai China

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/10.1029/2020GL087578

Reference52 articles.

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3. Beaulieu S.E. &Szafranski K.(2019).InterRidge global database of active submarine hydrothermal vent fields version 3.4. World Wide Web electronic publication available fromhttp://vents‐data.interridge.org

4. MAGNETIC ANOMALIES DUE TO PRISM‐SHAPED BODIES WITH ARBITRARY POLARIZATION

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