Oxidized iron in garnets from the mantle transition zone-Reference-Cited by-同舟云学术

Oxidized iron in garnets from the mantle transition zone

Published:2018-01-22 Issue:2 Volume:11 Page:144-147
ISSN:1752-0894
Container-title:Nature Geoscience
language:en
Short-container-title:Nature Geosci

Author:

Kiseeva Ekaterina S.^ORCID,Vasiukov Denis M.,Wood Bernard J.,McCammon Catherine^ORCID,Stachel Thomas,Bykov Maxim^ORCID,Bykova Elena^ORCID,Chumakov Aleksandr^ORCID,Cerantola Valerio,Harris Jeff W.,Dubrovinsky Leonid

Publisher

Springer Science and Business Media LLC

Subject

General Earth and Planetary Sciences

Link

http://www.nature.com/articles/s41561-017-0055-7.pdf

Reference45 articles.

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3. Wood, B. J., Bryndzia, L. T. & Johnson, K. E. Mantle oxidation state and its relationship to tectonic environment and fluid speciation. Science 248, 337–345 (1990).

4. Frost, D. J. & McCammon, C. A. The redox state of Earth's mantle. Annu. Rev. Earth Planet. Sci. 36, 389–420 (2008).

5. Woodland, A. B. & Koch, M. Variation in oxygen fugacity with depth in the upper mantle beneath the Kaapvaal craton, Southern Africa. Earth Planet. Sci. Lett. 214, 295–310 (2003).

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