The dunitic mantle-crust transition zone in the Oman ophiolite: Residue of melt-rock interaction, cumulates from high-mgo melts, or both?

Bénédicte Abily*, Georges Ceuleneer

*Corresponding author for this work

    Research output: Contribution to journal › Article › peer-review

    49 Citations (Scopus)

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    Earth & Environmental Sciences