-
- Yagi T.
- Institute for Solid State Physics, University of Tokyo
-
- Kondo T.
- Institute for Solid State Physics, University of Tokyo
-
- Funamori N.
- Institute for Solid State Physics, University of Tokyo
-
- Neill B. O'
- Institute for Solid State Physics, University of Tokyo
-
- Oguri K.
- Institute for Solid State Physics, University of Tokyo
-
- Mukaide T.
- Faculty of Science and Engineering, Chuo University
-
- Miyajima N.
- Department of Earth and Planetary Sciences, Hokkaido University
-
- Fujino K.
- Department of Earth and Planetary Sciences, Hokkaido University
書誌事項
- タイトル別名
-
- Post Garnet Phases and the Mineralogy o
この論文をさがす
抄録
Phase relations of garnet with variable compositions were studied using different types of high pressure apparatus and synchrotron radiation. The results of in situ X-ray observations and transmitting electron microscope (TEM) analysis of the recovered samples revealed that garnet first breakdown into an assemblage consisted of aluminous perovskite and other phase (s) under the lower mantle condition. The solubility of aluminum into the perovskite phase is likely to be enhanced by pressure and an existence of iron and calcium.
収録刊行物
-
- 高圧力の科学と技術
-
高圧力の科学と技術 7 6-8, 1998
日本高圧力学会
- Tweet
キーワード
詳細情報 詳細情報について
-
- CRID
- 1390282679358425600
-
- NII論文ID
- 10002688533
-
- NII書誌ID
- AN10452913
-
- ISSN
- 13481940
- 0917639X
-
- NDL書誌ID
- 4493822
-
- 本文言語コード
- en
-
- データソース種別
-
- JaLC
- NDL
- Crossref
- CiNii Articles
-
- 抄録ライセンスフラグ
- 使用不可