High-Pressure and High-Temperature in situ X-ray Diffraction Study of Natural Garnet(Mg_<0.72>Fe_<0.17>Ca_<0.11>)_3Al_2Si_3O_<12> up to 32 GPa and 2000 K Using MA8-Type Apparatus
スポンサーリンク
概要
著者
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Yagi T
Institute For Solid State Physics University Of Tokyo
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Uchida T.
Institute of Plasma Physics,Nagoya University,Nagoya
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YAGI T.
Institute for Solid State Physics, University of Tokyo
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FUNAMORI N.
Institute for Solid State Physics, University of Tokyo
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OGURI K.
Institute for Solid State Physics, University of Tokyo
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MIYAJIMA N.
Department of Earth and Planetary Sciences, Hokkaido University
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Funamori N.
Institute For Solid State Physics University Of Tokyo
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MIYAJIMA N.
Division of Earth and Planetary Sciences, Graduate School of Science, Hokkaido University
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FUJINO K.
Division of Earth and Planetary Sciences, Graduate School of Science, Hokkaido University
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Miyajima N.
Department Of Earth And Planetary Sciences Hokkaido University
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Oguri K.
Institute For Solid State Physics University Of Tokyo
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Fujino K
Department Of Earth And Planetary Sciences Hokkaido University
関連論文
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- Phase Transitions of MnO Under Static Compression
- Post Garnet Phases and the Mineralogy of the Lower Mantle
- High-Pressure and High-Temperature in situ X-ray Diffraction Study of Natural Garnet(Mg_Fe_Ca_)_3Al_2Si_3O_ up to 32 GPa and 2000 K Using MA8-Type Apparatus
- High-Pressure Synthesis and Magnetic Properties of Orthorhombic CuRh_2O_4(Condensed Matter : Electronic Structure, Electrical, Magnetic and Optical Properties)
- A17 Chemical Variation in the Unzen Magmas : a Perspective from Isotope Study
- Phase Transition of(Mg, Fe)SiO_3 Majorite