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瀬戸川帯静岡市二王山周辺域に産する斧石, ダトー石
https://doi.org/10.14945/00000362
https://doi.org/10.14945/00000362905cd505-dd96-438d-8080-84173b31f78e
名前 / ファイル | ライセンス | アクション |
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KJ00000102441.pdf (2.1 MB)
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Item type | 紀要論文 / Departmental Bulletin Paper(1) | |||||||
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公開日 | 2008-01-25 | |||||||
タイトル | ||||||||
タイトル | 瀬戸川帯静岡市二王山周辺域に産する斧石, ダトー石 | |||||||
言語 | ||||||||
言語 | jpn | |||||||
キーワード | ||||||||
主題Scheme | Other | |||||||
主題 | Setogawa Belt | |||||||
キーワード | ||||||||
主題Scheme | Other | |||||||
主題 | Mt. Nio slab | |||||||
キーワード | ||||||||
主題Scheme | Other | |||||||
主題 | axinite | |||||||
キーワード | ||||||||
主題Scheme | Other | |||||||
主題 | datolite | |||||||
キーワード | ||||||||
主題Scheme | Other | |||||||
主題 | subduction slab | |||||||
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 | |||||||
ID登録 | ||||||||
ID登録 | 10.14945/00000362 | |||||||
ID登録タイプ | JaLC | |||||||
タイトル(別言語) | ||||||||
その他のタイトル | The occurrences of axinite and datolite at Mt. Nio area in the Setogawa belts, Shizuoka, central Japan | |||||||
著者 |
平, 研介
× 平, 研介× 和田, 秀樹
WEKO
188
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書誌情報 |
静岡大学地球科学研究報告 巻 26, p. 39-49, 発行日 1999-07 |
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出版者 | ||||||||
出版者 | 静岡大学地球科学教室 | |||||||
NDC | ||||||||
主題Scheme | NDC | |||||||
主題 | 458 | |||||||
抄録 | ||||||||
内容記述タイプ | Abstract | |||||||
内容記述 | The occurrence, mineralogy and stable isotopic characteristics of axinite and datolite-bearing veins in the Mt. Nio area of the Setogawa Belt in Shizuoka were described. Along three valleys of Abe River (Kuchisenmata, Setozawa and Okunosawa), cobbles and outcrops of axinite bearing veins are found along fractures in greenrocks. Four outcrops of green-rocks at the valley head of Okunosawa, axinite bearing veins about 20cm in width and 1m in length were observed. Epidote, pargasite, calcite and quartz were observed in the axinite and datolite bearing veins. Carbon and oxygen isotopic values of calcites coexisting with axinite and datolite showed a nearly constant value for oxygen and were highly variable for carbon. This implied that the temperature of the hydrothermal water which formed these mineral veins was constant and the source of carbon in the hydrothermal fluid probably mixed with magmatic carbon and organic derived carbon accompanying the accretional processes of the Setogawa Belt. | |||||||
ISSN | ||||||||
収録物識別子タイプ | ISSN | |||||||
収録物識別子 | 03886298 | |||||||
NII論文ID | ||||||||
関連タイプ | isIdenticalTo | |||||||
識別子タイプ | NAID | |||||||
関連識別子 | 110000413389 | |||||||
NII書誌ID | ||||||||
収録物識別子タイプ | NCID | |||||||
収録物識別子 | AN00103190 | |||||||
フォーマット | ||||||||
内容記述タイプ | Other | |||||||
内容記述 | application/pdf | |||||||
著者版フラグ | ||||||||
出版タイプ | VoR | |||||||
出版タイプResource | http://purl.org/coar/version/c_970fb48d4fbd8a85 |