Search Results - Asafov, E.V.

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

    Belingwe komatiites (2.7Ga) originate from a plume with moderate water content, as inferred from inclusions in olivine by Asafov, E.V., Sobolev, A.V., Gurenko, A.A., Arndt, N.T., Batanova, V.G., Portnyagin, M.V., Garbe-Schönberg, D., Krasheninnikov, S.P.

    Published in Chemical geology
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