On the P–T– $$fO_{2}$$ f O 2 stability of Fe4O5, Fe5O6 and Fe4O5-rich solid solutions-Reference-Cited by-同舟云学术

On the P–T– $$fO_{2}$$ f O 2 stability of Fe4O5, Fe5O6 and Fe4O5-rich solid solutions

Published:2016-05 Issue:5 Volume:171 Page:
ISSN:0010-7999
Container-title:Contributions to Mineralogy and Petrology
language:en
Short-container-title:Contrib Mineral Petrol

Author:

Myhill Robert^ORCID,Ojwang Dickson O.,Ziberna Luca,Frost Daniel J.,Ballaran Tiziana Boffa,Miyajima Nobuyoshi

Funder

European Research Council

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics

Link

http://link.springer.com/content/pdf/10.1007/s00410-016-1258-4.pdf

Reference57 articles.

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2. Ballhaus C, Berry RF, Green DH (1991) High pressure experimental calibration of the olivine–orthopyroxene–spinel oxygen geobarometer: implications for the oxidation state of the upper mantle. Contrib Miner Petrol 107:27–40

3. Barin I (1989) Thermochemical data of pure substances, vol VII. VCH, Weinheim, FRG

4. Boffa Ballaran T, Uenver-Thiele L, Woodland AB (2015) Complete substitution of Fe2+ by Mg in Fe4O5: the crystal structure of the Mg2Fe2O5 end-member. Am Mineral 100:628–632

5. Bransky I, Hed AZ (1968) Thermogravimetric determination of the composition–oxygen partial pressure diagram of wustite (Fe1–yO). J Am Ceram Soc 51:231

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