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On the Significance of the Gneissic Rocks Found as Xenoliths in Andesite on the Sangun Metamorphic Belt of Yamaguchi Prefecture
https://doi.org/10.15027/53031
https://doi.org/10.15027/5303132a4ac0b-4219-4acd-8b46-028804d886f3
| 名前 / ファイル | ライセンス | アクション |
|---|---|---|
JSHUC_5-4_307.pdf (1.6 MB)
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| Item type | デフォルトアイテムタイプ_（フル）(1) | |||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|
| 公開日 | 2023-03-18 | |||||||||||
| タイトル | ||||||||||||
| タイトル | On the Significance of the Gneissic Rocks Found as Xenoliths in Andesite on the Sangun Metamorphic Belt of Yamaguchi Prefecture | |||||||||||
| 言語 | en | |||||||||||
| 作成者 |
KOJIMA, George
× KOJIMA, George
× NUREKI, Terukazu
× HASHIKAWA, Kunitaké
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| アクセス権 | ||||||||||||
| アクセス権 | open access | |||||||||||
| アクセス権URI | http://purl.org/coar/access_right/c_abf2 | |||||||||||
| 内容記述 | ||||||||||||
| 内容記述 | Gneissic rocks are found as xenoliths in the andesite of Mitakésan (Kimpôzan), 15 km to the north-northeast of Tokuyama City, Yamaguchi Prefecture. The xenoliths consist mainly of gneisses derived from basic rocks, containing hornblende, biotite, and plagioclase, in some specimens with clinopyroxene. Quartzo-feldspathic gneisses, consisting of biotite, plagioclase, and quartz, sometimes with garnet, pelitic gneiss, and non-foliated magmatites are also included. Judged from their rock association and mineral assemblage, they cannot be correlated to the gneisses either of the Ryôké or the Sangun metamorphic complex. The occurrence of gneiss xenoliths testifies to the presence of sialic layer, underlying the Sangun crystalline schists, which are characterized by the nature of the glaucophanitic metamorphism. | |||||||||||
| 言語 | en | |||||||||||
| 出版者 | ||||||||||||
| 出版者 | HIROSHIMA UNIVERSITY | |||||||||||
| 言語 | ||||||||||||
| 言語 | eng | |||||||||||
| 資源タイプ | ||||||||||||
| 資源タイプ識別子 | http://purl.org/coar/resource_type/c_6501 | |||||||||||
| 資源タイプ | departmental bulletin paper | |||||||||||
| 出版タイプ | ||||||||||||
| 出版タイプ | VoR | |||||||||||
| 出版タイプResource | http://purl.org/coar/version/c_970fb48d4fbd8a85 | |||||||||||
| ID登録 | ||||||||||||
| ID登録 | 10.15027/53031 | |||||||||||
| ID登録タイプ | JaLC | |||||||||||
| 収録物識別子 | ||||||||||||
| 収録物識別子タイプ | ISSN | |||||||||||
| 収録物識別子 | 0075-4374 | |||||||||||
| 収録物識別子 | ||||||||||||
| 収録物識別子タイプ | NCID | |||||||||||
| 収録物識別子 | AA00706718 | |||||||||||
| 開始ページ | ||||||||||||
| 開始ページ | 307 | |||||||||||
| 書誌情報 |
Journal of science of the Hiroshima University. Series C, Geology and mineralogy Journal of science of the Hiroshima University. Series C, Geology and mineralogy 巻 5, 号 4, p. 307-310, 発行日 1968-03-31 |
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| 旧ID | 53031 | |||||||||||
