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Iron-rich silicates in the Earth's D″ layer
High-pressure experiments and theoretical calculations demonstrate that an iron-rich ferromagnesian silicate phase can be synthesized at the pressure–temperature conditions near the core–mantle boundary. The iron-rich phase is up to 20% denser than any known silicate at the core–mantle boundary. The...
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Main Authors: | , , , , , , , , , , , |
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Formato: | Artigo |
Idioma: | Inglês |
Publicado em: |
National Academy of Sciences
2005
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Assuntos: | |
Acesso em linha: | https://ncbi.nlm.nih.gov/pmc/articles/PMC1174998/ https://ncbi.nlm.nih.gov/pubmed/15994226 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.0503737102 |
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