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Pyritic Ore, Deposits of the Yanahara District, Japan
https://doi.org/10.15027/52994
https://doi.org/10.15027/529948bb52bfc-dc9f-4103-b2af-f15413918828
| 名前 / ファイル | ライセンス | アクション |
|---|---|---|
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| Item type | デフォルトアイテムタイプ_(フル)(1) | |||||||
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| 公開日 | 2023-03-18 | |||||||
| タイトル | ||||||||
| タイトル | Pyritic Ore, Deposits of the Yanahara District, Japan | |||||||
| 言語 | en | |||||||
| 作成者 |
HIGASHIMOTO, Sadao
× HIGASHIMOTO, Sadao
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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 | The ores of the Yanahara Mine, which has hitherto been widely noted for its leading pro-duction of iron sulphide ore in Japan, are deposited only in the ‘Yanahara complex' correlative to a member of the upper Permian including a complicated alternation of acidic tuff, slate, rhyolite, dacite, and so forth. Modes of their occurrence are classified into two types such as the massive, and the disseminated ores, of which the former involves mainly pyrite together with pyrrhotite and magnetite. The pyrite ore contained conformably in the Yanahara complex seems to have been formed through low-temperature hydro-thermal replacement accompanied subsequently with cataclastic, and then thermal metamorphisms. The magnetite, and pyrrhotite ores are found concentrated around pyrite ore bodies and along the fractures cutting across the latter or along quartz porphyry dike, showing no evidence for metamorphism in their textures. Most of these ores seem to have been derived from interaction of the pyrite ore with hydrothermal solution ascending along the fissures distributed around or in the pre-existing pyrite ore bodies, and the formation of some of the pyrrhotite ore related to dikes might have been ascribed to thermal metamorphism. | |||||||
| 言語 | en | |||||||
| 内容記述 | ||||||||
| 内容記述タイプ | Other | |||||||
| 内容記述 | Thesis presented for the degree of D. Sc. of the Hiroshima University. | |||||||
| 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 | 10.15027/52994 | |||||||
| 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 | 25 | |||||||
| 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 3, 号 1, p. 25-68, 発行日 1960-03-25 |
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| 旧ID | 52994 | |||||||