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The role of the antigorite + brucite to olivine reaction in subducted serpentinites (Zermatt, Switzerland)
Metamorphic olivine formed by the reaction of antigorite + brucite is widespread in serpentinites that crop out in glacier-polished outcrops at the Unterer Theodulglacier, Zermatt. Olivine overgrows a relic magnetite mesh texture formed during ocean floor serpentinization. Serpentinization is associ...
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| Publié dans: | Swiss J Geosci |
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| Auteurs principaux: | , , , , |
| Format: | Artigo |
| Langue: | Inglês |
| Publié: |
Springer International Publishing
2020
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| Sujets: | |
| Accès en ligne: | https://ncbi.nlm.nih.gov/pmc/articles/PMC7588401/ https://ncbi.nlm.nih.gov/pubmed/33132816 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1186/s00015-020-00368-0 |
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