Hydrous peridotitic fragments of Earth’s mantle 660 km discontinuity sampled by a diamond-Reference-Cited by-同舟云学术

Hydrous peridotitic fragments of Earth’s mantle 660 km discontinuity sampled by a diamond

Published:2022-09-26 Issue:11 Volume:15 Page:950-954
ISSN:1752-0894
Container-title:Nature Geoscience
language:en
Short-container-title:Nat. Geosci.

Author:

Gu Tingting^ORCID,Pamato Martha G.^ORCID,Novella Davide^ORCID,Alvaro Matteo^ORCID,Fournelle John,Brenker Frank E.^ORCID,Wang Wuyi^ORCID,Nestola Fabrizio^ORCID

Publisher

Springer Science and Business Media LLC

Subject

General Earth and Planetary Sciences

Link

https://www.nature.com/articles/s41561-022-01024-y.pdf

Reference77 articles.

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2. Fei, H. & Katsura, T. Water solubility in Fe‐bearing wadsleyite at mantle transition zone temperatures. Geophys. Res. Lett. 48, e2021GL092836 (2021).

3. Ito, E. & Takahashi, E. Postspinel transformations in the system Mg2SiO4–Fe2SiO4 and some geophysical implications. J. Geophys. Res. Solid Earth 94, 10637–10646 (1989).

4. Bolfan-Casanova, N. Water in the Earth’s mantle. Mineral. Mag. 69, 229–258 (2005).

5. Litasov, K. et al. Water solubility in Mg-perovskites and water storage capacity in the lower mantle. Earth Planet. Sci. Lett. 211, 189–203 (2003).

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