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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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Detalhes bibliográficos
Main Authors: Mao, Wendy L., Meng, Yue, Shen, Guoyin, Prakapenka, Vitali B., Campbell, Andrew J., Heinz, Dion L., Shu, Jinfu, Caracas, Razvan, Cohen, Ronald E., Fei, Yingwei, Hemley, Russell J., Mao, Ho-kwang
Formato: Artigo
Idioma:Inglês
Publicado em: National Academy of Sciences 2005
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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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