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Recovery of an oxidized majorite inclusion from Earth’s deep asthenosphere
Minerals recovered from the deep mantle provide a rare glimpse into deep Earth processes. We report the first discovery of ferric iron–rich majoritic garnet found as inclusions in a host garnet within an eclogite xenolith originating in the deep mantle. The composition of the host garnet indicates a...
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| Опубликовано в: : | Sci Adv |
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| Главные авторы: | , , , , , , , |
| Формат: | Artigo |
| Язык: | Inglês |
| Опубликовано: |
American Association for the Advancement of Science
2017
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| Предметы: | |
| Online-ссылка: | https://ncbi.nlm.nih.gov/pmc/articles/PMC5384806/ https://ncbi.nlm.nih.gov/pubmed/28435871 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1126/sciadv.1601589 |
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