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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 |
完全メタデータレコード
| DCフィールド | 値 | 言語 |
|---|---|---|
| dc.contributor.author | SHIMADA, Mitsuhiko | en |
| dc.date.accessioned | 2013-09-02T04:22:25Z | - |
| dc.date.available | 2013-09-02T04:22:25Z | - |
| dc.date.issued | 1967-12 | - |
| dc.identifier.issn | 0454-7837 | - |
| dc.identifier.uri | http://hdl.handle.net/2433/178530 | - |
| dc.description.abstract | 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. | en |
| dc.format.mimetype | application/pdf | - |
| dc.language.iso | eng | - |
| dc.publisher | Geophysical Institute, Kyoto University | en |
| dc.subject.ndc | 450 | - |
| dc.title | AN EXPERIMENTAL STUDY OF THE BASALT-ECLOGITE TRANSITION | en |
| dc.type | departmental bulletin paper | - |
| dc.type.niitype | Departmental Bulletin Paper | - |
| dc.identifier.ncid | AA00423961 | - |
| dc.identifier.jtitle | Special Contributions of the Geophysical Institute, Kyoto University | en |
| dc.identifier.volume | 7 | - |
| dc.identifier.spage | 211 | - |
| dc.identifier.epage | 217 | - |
| dc.textversion | publisher | - |
| dc.sortkey | 24 | - |
| dcterms.accessRights | open access | - |
| dc.identifier.pissn | 0454-7837 | - |
| 出現コレクション: | No.7 | |
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