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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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Bibliografische gegevens
Gepubliceerd in:Boletín de la Sociedad Geológica Mexicana
Hoofdauteurs: José M. González-Jiménez, Ivanina Sergeeva, Thomas N. Kerestedjian, Fernando Gervilla
Formaat: Artigo
Taal:Inglês
Gepubliceerd in: Sociedad Geológica Mexicana, A.C. 2022
Onderwerpen:
Online toegang: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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