From magma ocean to core-mantle boundary:the key role of hydrous ferropericlase in shaping deep Earth's low-velocity anomaliesOA
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
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,ChinaState Key Laboratory of Deep Earth Processes and Resources,Guangzhou Institute of Geochemistry,Chinese Academy of Sciences,ChinaState Key Laboratory of Deep Earth Processes and Resources,Guangzhou Institute of Geochemistry,Chinese Academy of Sciences,ChinaDepartment of Chemistry and Molecular Biology,University of Gothenburg,SwedenState Key Laboratory of Deep Earth Processes and Resources,Guangzhou Institute of Geochemistry,Chinese Academy of Sciences,China
《国家科学评论（英文版）》 2026 (9)
24-27,4
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).
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