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Subducted iron and glassy spherules in the upper mantle?
Spherules are documented in ophiolitic mantle rocks such as peridotites and associated chromitites. They consist of: (1) native iron having variable amounts of Ni with/without inclusions of silicate glass or oxides (wüstite), (2) dendritic intergrowth of oxides (magnetite, wüstite and hematite) with...
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| Publié dans: | Boletín de la Sociedad Geológica Mexicana |
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| Auteurs principaux: | , , , |
| Format: | Artigo |
| Langue: | Inglês |
| Publié: |
Sociedad Geológica Mexicana, A.C.
2022
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| Sujets: | |
| Accès en ligne: | https://www.redalyc.org/articulo.oa?id=94375433014 |
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