Subduction-related oxidation of the sublithospheric mantle evidenced by ferropericlase and magnesiowüstite diamond inclusions

Ferropericlase (Mg,Fe)O is the second most abundant mineral in Earth’s lower mantle and a common inclusion found in subcratonic diamonds. Pyrolitic mantle has Mg# (100 × Mg/(Mg+Fe)) ~89. However, ferropericlase inclusions in diamonds show a broad range of Mg# between 12 and 93. Here we use Synchrotr...

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Detalles Bibliográficos
Autores principales: Kiseeva, Ekaterina S., Korolev, Nester, Koemets, Iuliia, Zedgenizov, Dmitry A., Unitt, Richard, McCammon, Catherine, Aslandukova, Alena, Khandarkhaeva, Saiana, Fedotenko, Timofey, Glazyrin, Konstantin, Bessas, Dimitrios, Aprilis, Georgios, Chumakov, Alexandr I., Kagi, Hiroyuki, Dubrovinsky, Leonid
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2022
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9726884/
https://www.ncbi.nlm.nih.gov/pubmed/36473837
http://dx.doi.org/10.1038/s41467-022-35110-x

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9726884/
https://www.ncbi.nlm.nih.gov/pubmed/36473837
http://dx.doi.org/10.1038/s41467-022-35110-x

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