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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...
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 |
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Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
Nature Publishing Group UK
2022
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Materias: | |
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 |
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