Peridotites and basalts reveal broad congruence between two independent records of mantle fO2 despite local redox heterogeneity-Reference-Cited by-同舟云学术

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Peridotites and basalts reveal broad congruence between two independent records of mantle fO2 despite local redox heterogeneity

Published:2018-07 Issue: Volume:494 Page:172-189
ISSN:0012-821X
Container-title:Earth and Planetary Science Letters
language:en
Short-container-title:Earth and Planetary Science Letters

Author:

Birner Suzanne K.^ORCID,Cottrell Elizabeth,Warren Jessica M.^ORCID,Kelley Katherine A.^ORCID,Davis Fred A.

Funder

National Science Foundation

U.S. Department of Energy (DOE) – Geosciences

University of Chicago – CARS

U.S. Department of Energy (DOE) Office of Science

National Science Foundation – Earth Sciences

U.S. Department of Energy – GeoSciences

DOE Office of Science by Argonne National Laboratory

Publisher

Elsevier BV

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Reference88 articles.

1. The Fe3+/ΣFe ratios of MORB glasses and their implications for mantle melting;Bézos;Geochim. Cosmochim. Acta,2005

2. Hydrothermal alteration of seafloor peridotites does not influence oxygen fugacity recorded by spinel oxybarometry;Birner;Geology,2016

3. Forearc peridotites from Tonga record heterogeneous oxidation of the mantle following subduction initiation;Birner;J. Petrol.,2017

4. The stability of plagioclase in the upper mantle: subsolidus experiments on fertile and depleted lherzolite;Borghini;J. Petrol.,2010

5. Geothermobarometry in four-phase lherzolites II. New thermobarometers, and practical assessment of existing thermobarometers;Brey;J. Petrol.,1990

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