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Pressure-induced structural change in MgSiO(3) glass at pressures near the Earth’s core–mantle boundary

Knowledge of the structure and properties of silicate magma under extreme pressure plays an important role in understanding the nature and evolution of Earth’s deep interior. Here we report the structure of MgSiO(3) glass, considered an analog of silicate melts, up to 111 GPa. The first (r1) and sec...

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Bibliografski detalji
Izdano u:Proc Natl Acad Sci U S A
Glavni autori: Kono, Yoshio, Shibazaki, Yuki, Kenney-Benson, Curtis, Wang, Yanbin, Shen, Guoyin
Format: Artigo
Jezik:Inglês
Izdano: National Academy of Sciences 2018
Teme:
Online pristup:https://ncbi.nlm.nih.gov/pmc/articles/PMC5828608/
https://ncbi.nlm.nih.gov/pubmed/29432162
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.1716748115
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