WEKO3
アイテム
Pressure-Temperature-Water Production Rate Paths in the Subduction Metamorphism
https://doi.org/10.15083/0000032610
https://doi.org/10.15083/000003261061cc42c8-fe5f-4d7c-b9ae-765251facde8
| 名前 / ファイル | ライセンス | アクション |
|---|---|---|
ji0763009.pdf (1.1 MB)
|
|
| Item type | 紀要論文 / Departmental Bulletin Paper(1) | |||||
|---|---|---|---|---|---|---|
| 公開日 | 2008-05-30 | |||||
| タイトル | ||||||
| タイトル | Pressure-Temperature-Water Production Rate Paths in the Subduction Metamorphism | |||||
| 言語 | en | |||||
| 言語 | ||||||
| 言語 | eng | |||||
| キーワード | ||||||
| 主題Scheme | Other | |||||
| 主題 | metamorphism | |||||
| キーワード | ||||||
| 主題Scheme | Other | |||||
| 主題 | dehydration | |||||
| キーワード | ||||||
| 主題Scheme | Other | |||||
| 主題 | water release | |||||
| キーワード | ||||||
| 主題Scheme | Other | |||||
| 主題 | subduction | |||||
| 資源タイプ | ||||||
| 資源 | http://purl.org/coar/resource_type/c_6501 | |||||
| タイプ | departmental bulletin paper | |||||
| ID登録 | ||||||
| ID登録 | 10.15083/0000032610 | |||||
| ID登録タイプ | JaLC | |||||
| その他のタイトル | ||||||
| その他のタイトル | 沈み込み変成作用の圧力-温度-水生成量 | |||||
| 著者 |
Toriumi, Mitsuhiro
× Toriumi, Mitsuhiro× Inui, Mutsuko |
|||||
| 著者別名 | ||||||
| 識別子Scheme | WEKO | |||||
| 識別子 | 126190 | |||||
| 姓名 | 鳥海, 光弘 | |||||
| 著者別名 | ||||||
| 識別子Scheme | WEKO | |||||
| 識別子 | 126191 | |||||
| 姓名 | 乾, 睦子 | |||||
| 著者所属 | ||||||
| 著者所属 | Graduate School of Frontier Sciences, University of Tokyo, and Jamstec, Integrated Frontier Research Institute of Earth Evolution | |||||
| 著者所属 | ||||||
| 著者所属 | Department of Technology, Kokusikan University | |||||
| 抄録 | ||||||
| 内容記述タイプ | Abstract | |||||
| 内容記述 | Metamorphic pressure and temperature paths were precisely inferred by chemical zonal structure of garnet from the core to the rim in pelitic systems using the differential thermodynamic method. We obtained P-T paths from the Sambagawa metamorphism such that the pressure and temperature increased gradually during the growth of garnet. The zonal structures of garnet show a continuous change of pressure and temperature but indicate wide variations in the garnet production rate. The molar production rates of garnet during prograde metamorphism, denned by dm/dP were precisely obtained, in which m is the molar production of garnet normalized by the grain volume. The rates commonly show two peaks near the early and late stages. The general trends of molar production rates show a gradual increase with increasing pressure, but there are several peaks and the rates suggest episodic water release from metamorphic rocks in the process of subduction. | |||||
| 書誌情報 |
東京大學地震研究所彙報 = Bulletin of the Earthquake Research Institute, University of Tokyo 巻 76, 号 3, p. 367-376, 発行日 2002-02-12 |
|||||
| ISSN | ||||||
| 収録物識別子タイプ | ISSN | |||||
| 収録物識別子 | 00408972 | |||||
| 書誌レコードID | ||||||
| 収録物識別子タイプ | NCID | |||||
| 収録物識別子 | AN00162258 | |||||
| フォーマット | ||||||
| 内容記述タイプ | Other | |||||
| 内容記述 | application/pdf | |||||
| 日本十進分類法 | ||||||
| 主題Scheme | NDC | |||||
| 主題 | 458 | |||||
| 出版者 | ||||||
| 出版者 | 東京大学地震研究所 | |||||
| 出版者別名 | ||||||
| Earthquake Research Institute, University of Tokyo | ||||||
