Gagarinite-type Fe <sub>2.5</sub> (OH) <sub>6</sub> under the deep lower mantle conditions
may contribute to chemical heterogeneities in the bottom 1,000 km of the mantle and explain some of the complex seismic anomalies.
Authors
- Ho‐kwang Mao (ORCID: https://orcid.org/0000-0002-0481-5683)
- Li Zhang (ORCID: https://orcid.org/0000-0003-2684-6832)
- Ziqiang Yang (ORCID: https://orcid.org/0000-0003-3920-744X)
Institutions
- Center for High Pressure Science and Technology Advanced Research (CN)
Publication Details
- Journal
- Proceedings of the National Academy of Sciences
- Published
- 2026-04-22
- DOI
- https://doi.org/10.1073/pnas.2603677123
- Primary Topic
- High-pressure geophysics and materials
- Type
- article
- Field-Weighted Citation Impact
- 0.00
Funders
- National Natural Science Foundation of China