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Redox state of the convective mantle from CO2-trace element systematics of oceanic basalts
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1Department of Earth, Environmental and Planetary Sciences, Rice University, 6100 Main Street, MS 126, Houston, TX 77005
Eguchi, J., Dasgupta, R. (2018) Redox state of the convective mantle from CO2-trace element systematics of oceanic basalts. Geochem. Persp. Let. 8, 17–21.
NSF grants EAR-1255391, OCE-1338842, and the Sloan Foundation through Deep Carbon Observatory.
Geochemical Perspectives Letters v8 | doi: 10.7185/geochemlet.1823
Received 20 April 2018 | Accepted 01 August 2018 | Published 18 September 2018
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Published by the European Association of Geochemistry
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