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西南日本,広島県と島根県下に分布する花崗岩中に見られる粘土細脈と粘土鉱物
https://hiroshima.repo.nii.ac.jp/records/2005276
https://hiroshima.repo.nii.ac.jp/records/20052763fe2cd53-13e7-40f4-b00f-6b3abb5a5977
| 名前 / ファイル | ライセンス | アクション |
|---|---|---|
diss_otsu1408.pdf (5.1 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 | Clay Veins and Clay Minerals in the Granitic Rocks in Hiroshima and Shimane Prefectures, Southwest Japan : Effect of the hydrothermal activities on the decomposition of the granitic rocks | |||||||||
| 言語 | en | |||||||||
| タイトル | ||||||||||
| タイトル | 西南日本,広島県と島根県下に分布する花崗岩中に見られる粘土細脈と粘土鉱物 | |||||||||
| 言語 | ja | |||||||||
| 作成者 |
北川, 隆司
× 北川, 隆司
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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 | |||||||||
| 権利情報 | ||||||||||
| 権利情報 | Copyright(c) by Author | |||||||||
| 主題 | ||||||||||
| 主題Scheme | NDC | |||||||||
| 主題 | 450 | |||||||||
| 内容記述 | ||||||||||
| 内容記述 | This paper deals with the clay minerals found in the granitic rocks distributed in Hiroshima and Shimane Prefectures with special reference to the effects of hydrothermal activities on the decomposition process of the granitic rocks. Many clay veins and hydrothermal clay deposits are commonly developed in the granitic rocks and their mode of occurrences were investigated in detail. the preferred orientations of the clay veins and microcracks found in the constituent minerals of granitic rocks were examined. The constituent clay minerals and their mineralogical characteristics of clay veins, clay deposits and alteration products of plagioclase in granitic rocks were investigated by means of X-ray diffraction, optical microscope, electron microscope(TEM and SEM), hydrogen isotope ratio and so on. The major results obtained are as follows. 1)The preferred orientations of microcracks within granitic rocks are very similar to those of clay veins which have been formed under the regional compression stress field. 2)Theconstituent clay mnerals of clay veins, clay deposits and alteration peoducts from plagioclase and theie mineralogical characteristics are almost identical with each other. 3)Mineral sequence found in the vertical direction of a clay vein and altered granitic rocks resemble to that ovserved in some present geothermal areas. 4)Mineralogical characteristics of the clay minerals indicate that the clay minerals were formed by hydrothermal solution subsequent to the post granitic activity. The temperature of hydrothermal solution ranges about 50゜-300゜ C and originated from meteoric water. Some clay minerals seem tobe directly precipitated from the hydrothemal solution. Based on the results mentioned above, it is considered that granitic rocks distributed in the investigated areas have been strongly fractured and characterized by remarkable alteration to clay minerals at hydrothermal stage before the weathering stage. | |||||||||
| 言語 | en | |||||||||
| 内容記述 | ||||||||||
| 内容記述タイプ | Other | |||||||||
| 内容記述 | Journal of Science of the Hiroshima University, Series C, Vol.9, No.1 (1986) pp. 47-80 | |||||||||
| 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_db06 | |||||||||
| 資源タイプ | doctoral thesis | |||||||||
| 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 | 47 | |||||||||
| 書誌情報 |
巻 9, 号 1, p. 47-80 |
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| 学位授与番号 | ||||||||||
| 学位授与番号 | 乙第1408号 | |||||||||
| 学位名 | ||||||||||
| 言語 | ja | |||||||||
| 学位名 | 博士(理学) | |||||||||
| 学位名 | ||||||||||
| 言語 | en | |||||||||
| 学位名 | Physical Science | |||||||||
| 学位授与年月日 | ||||||||||
| 学位授与年月日 | 1986-02-24 | |||||||||
| 学位授与機関 | ||||||||||
| 学位授与機関識別子Scheme | kakenhi | |||||||||
| 学位授与機関識別子 | 15401 | |||||||||
| 言語 | ja | |||||||||
| 学位授与機関名 | 広島大学 | |||||||||
| 学位授与機関 | ||||||||||
| 言語 | en | |||||||||
| 学位授与機関名 | Hiroshima University | |||||||||
| 旧ID | 20974 | |||||||||
