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Diamond formation in the deep lower mantle: a high-pressure reaction of MgCO(3) and SiO(2)

Diamond is an evidence for carbon existing in the deep Earth. Some diamonds are considered to have originated at various depth ranges from the mantle transition zone to the lower mantle. These diamonds are expected to carry significant information about the deep Earth. Here, we determined the phase...

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Detalhes bibliográficos
Publicado no:Sci Rep
Main Authors: Maeda, Fumiya, Ohtani, Eiji, Kamada, Seiji, Sakamaki, Tatsuya, Hirao, Naohisa, Ohishi, Yasuo
Formato: Artigo
Idioma:Inglês
Publicado em: Nature Publishing Group 2017
Assuntos:
Acesso em linha:https://ncbi.nlm.nih.gov/pmc/articles/PMC5233982/
https://ncbi.nlm.nih.gov/pubmed/28084421
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/srep40602
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