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Depth-dependent peridotite-melt interaction and the origin of variable silica in the cratonic mantle

Peridotites from the thick roots of Archaean cratons are known for their compositional diversity, whose origin remains debated. We report thermodynamic modelling results for reactions between peridotite and ascending mantle melts. Reaction between highly magnesian melt (komatiite) and peridotite lea...

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Détails bibliographiques
Publié dans:Nat Commun
Auteurs principaux: Tomlinson, Emma L., Kamber, Balz S.
Format: Artigo
Langue:Inglês
Publié: Nature Publishing Group UK 2021
Sujets:
Accès en ligne:https://ncbi.nlm.nih.gov/pmc/articles/PMC7889928/
https://ncbi.nlm.nih.gov/pubmed/33597517
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/s41467-021-21343-9
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