From magma ocean to core–mantle boundary: the key role of hydrous ferropericlase in shaping deep Earth’s low-velocity anomalies
- 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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Cite this work
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
Source records
- crossref · retrieved 2026-09-27T11:02:26.745Z