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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...
| Autores principales: | , , , , , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
| Publicado: |
Nature Publishing Group
2017
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| Materias: | |
| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5233982/ https://www.ncbi.nlm.nih.gov/pubmed/28084421 http://dx.doi.org/10.1038/srep40602 |