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このアイテムのファイル:
| ファイル | 記述 | サイズ | フォーマット | |
|---|---|---|---|---|
| sgk00700_211.pdf | 491.04 kB | Adobe PDF | 見る/開く |
| タイトル: | AN EXPERIMENTAL STUDY OF THE BASALT-ECLOGITE TRANSITION |
| 著者: | SHIMADA, Mitsuhiko |
| 発行日: | Dec-1967 |
| 出版者: | Geophysical Institute, Kyoto University |
| 誌名: | Special Contributions of the Geophysical Institute, Kyoto University |
| 巻: | 7 |
| 開始ページ: | 211 |
| 終了ページ: | 217 |
| 抄録: | The basalt-eclogite transition has been investigated experimentally using natural basalt as the starting material. Temperature interval investigated in this work was not so wide (from the solidus of the basalt to 850°C) that the stability lines extrapolated to lower temperatures has large ambiguity. In spite of this large ambiguity, the result shows that the possibility that the Mohorovicic discontinuity under the continent is caused by the basalt-eclogite transition is not entirely rejected. |
| URI: | http://hdl.handle.net/2433/178530 |
| 出現コレクション: | No.7 |
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