Ferromagnesian postperovskite silicates in the D″ layer of the Earth

Natural olivine with 12 mol % Fe(2)SiO(4) and synthetic orthopyroxenes with 20% and 40% FeSiO(3) were studied beyond the pressure–temperature conditions of the core–mantle boundary. All samples were found to convert entirely or partially into the CaIrO(3) postperovskite structure, which was recently...

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Detaylı Bibliyografya
Asıl Yazarlar: Mao, Wendy L., Shen, Guoyin, Prakapenka, Vitali B., Meng, Yue, Campbell, Andrew J., Heinz, Dion L., Shu, Jinfu, Hemley, Russell J., Mao, Ho-kwang
Materyal Türü: Artigo
Dil:Inglês
Baskı/Yayın Bilgisi: National Academy of Sciences 2004
Konular:
Physical Sciences
Online Erişim:https://ncbi.nlm.nih.gov/pmc/articles/PMC528774/
https://ncbi.nlm.nih.gov/pubmed/15520393
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.0407135101
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