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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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| Udgivet i: | Nat Commun |
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| Main Authors: | , |
| Format: | Artigo |
| Sprog: | Inglês |
| Udgivet: |
Nature Publishing Group UK
2021
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| Fag: | |
| Online adgang: | 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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