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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| I publikationen: | Boletín de la Sociedad Geológica Mexicana |
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| Huvudupphov: | , , , |
| Materialtyp: | Artigo |
| Språk: | Inglês |
| Utgiven: |
Sociedad Geológica Mexicana, A.C.
2022
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| Ämnen: | |
| Länkar: | https://www.redalyc.org/articulo.oa?id=94375433014 https://www.redalyc.org/journal/943/94375433014/ https://www.redalyc.org/journal/943/94375433014/html/ https://www.redalyc.org/journal/943/94375433014/94375433014.epub https://www.redalyc.org/journal/943/94375433014/movil https://doi.org/10.18268/BSGM2022v74n3a200722 |
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