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

Open source

DOI
10.1093/nsr/nwag258
Published
2026-05-01
Container
National Science Review
Publisher
Oxford University Press (OUP)
Open access
unknown

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BibTeX

@article{allodium:10.1093/nsr/nwag258,
  title = {From magma ocean to core–mantle boundary: the key role of hydrous ferropericlase in shaping deep Earth’s low-velocity anomalies},
  author = {Shi-Dong Guan and Yu Wang and Zhi-Xue Du and Ya-Nan Yang and Yi-Gang Xu},
  year = {2026},
  journal = {National Science Review},
  doi = {10.1093/nsr/nwag258},
  url = {https://doi.org/10.1093/nsr/nwag258}
}

RIS

TY  - JOUR
TI  - From magma ocean to core–mantle boundary: the key role of hydrous ferropericlase in shaping deep Earth’s low-velocity anomalies
AU  - Shi-Dong Guan
AU  - Yu Wang
AU  - Zhi-Xue Du
AU  - Ya-Nan Yang
AU  - Yi-Gang Xu
PY  - 2026
JO  - National Science Review
DO  - 10.1093/nsr/nwag258
UR  - https://doi.org/10.1093/nsr/nwag258
ER  - 

APA

Guan, S., Wang, Y., Du, Z., Yang, Y., & Xu, Y. (2026). From magma ocean to core–mantle boundary: the key role of hydrous ferropericlase in shaping deep Earth’s low-velocity anomalies. National Science Review. https://doi.org/10.1093/nsr/nwag258

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