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 journalArticlepeer-review

    49 Citations (Scopus)

    Fingerprint

    Dive into the research topics of 'The dunitic mantle-crust transition zone in the Oman ophiolite: Residue of melt-rock interaction, cumulates from high-mgo melts, or both?'. Together they form a unique fingerprint.

    Earth & Environmental Sciences