Belingwe komatiites (2.7 Ga) originate from a plume with moderate water content, as inferred from inclusions in olivine-Reference-Cited by-同舟云学术

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Belingwe komatiites (2.7 Ga) originate from a plume with moderate water content, as inferred from inclusions in olivine

Published:2018-02 Issue: Volume:478 Page:39-59
ISSN:0009-2541
Container-title:Chemical Geology
language:en
Short-container-title:Chemical Geology

Author:

Asafov E.V.,Sobolev A.V.,Gurenko A.A.,Arndt N.T.,Batanova V.G.,Portnyagin M.V.,Garbe-Schönberg D.,Krasheninnikov S.P.

Funder

Russian Science Foundation

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference86 articles.

1. Genesis of Archaean komatiites in a wet ultramafic subducted plate;Allègre,1982

2. Were komatiites wet?;Arndt;Geology,1998

3. Komatiite;Arndt,2008

4. High pressure experimental calibration of the olivine-orthopyroxene-spinel oxygen geobarometer: implications for the oxidation state of the upper mantle;Ballhaus;Contrib. Mineral. Petrol.,1991

5. Chromite in komatiites, 1. Magmatic controls on crystallization and composition;Barnes;J. Petrol.,1998

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