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From magma ocean to core-mantle boundary:the key role of hydrous ferropericlase in shaping deep Earth's low-velocity anomalies

Shi-Dong Guan Yu Wang Zhi-Xue Du Ya-Nan Yang Yi-Gang Xu

国家科学评论（英文版）2026，Vol.13Issue(9)：24-27,4.

国家科学评论（英文版）2026，Vol.13Issue(9)：24-27,4.DOI:10.1093/nsr/nwag258

From magma ocean to core-mantle boundary:the key role of hydrous ferropericlase in shaping deep Earth's low-velocity anomalies

Shi-Dong Guan ¹Yu Wang ²Zhi-Xue Du ²Ya-Nan Yang ³Yi-Gang Xu²

作者信息

1. State Key Laboratory of Deep Earth Processes and Resources,Guangzhou Institute of Geochemistry,Chinese Academy of Sciences,China||College of Earth and Planetary Sciences,University of Chinese Academy of Sciences,China
2. State Key Laboratory of Deep Earth Processes and Resources,Guangzhou Institute of Geochemistry,Chinese Academy of Sciences,China
3. Department of Chemistry and Molecular Biology,University of Gothenburg,Sweden
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摘要

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Shi-Dong Guan,Yu Wang,Zhi-Xue Du,Ya-Nan Yang,Yi-Gang Xu..From magma ocean to core-mantle boundary:the key role of hydrous ferropericlase in shaping deep Earth's low-velocity anomalies[J].国家科学评论（英文版）,2026,13(9):24-27,4.

基金项目

This work was supported by the National Key R&D Program of China(2022YFF0801001),and the Strategic Priority Research Program of the Chinese Academy of Sciences(XDB0840200). （2022YFF0801001）

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