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Transportation of H2O and Melting beneath the Japan Arcs
https://doi.org/10.15083/0000032611
https://doi.org/10.15083/000003261150e8c8ea-1c9e-4c57-b4f6-11c736578a1b
| 名前 / ファイル | ライセンス | アクション |
|---|---|---|
ji0763010.pdf (1.6 MB)
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| Item type | 紀要論文 / Departmental Bulletin Paper(1) | |||||
|---|---|---|---|---|---|---|
| 公開日 | 2008-05-30 | |||||
| タイトル | ||||||
| タイトル | Transportation of H2O and Melting beneath the Japan Arcs | |||||
| 言語 | en | |||||
| 言語 | ||||||
| 言語 | eng | |||||
| キーワード | ||||||
| 主題Scheme | Other | |||||
| 主題 | H2O | |||||
| キーワード | ||||||
| 主題Scheme | Other | |||||
| 主題 | melt | |||||
| キーワード | ||||||
| 主題Scheme | Other | |||||
| 主題 | subduction | |||||
| キーワード | ||||||
| 主題Scheme | Other | |||||
| 主題 | Japan arcs | |||||
| 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 | 10.15083/0000032611 | |||||
| ID登録タイプ | JaLC | |||||
| その他のタイトル | ||||||
| その他のタイトル | 日本弧下の水の輸送と溶融 | |||||
| 著者 |
Iwamori, Hikaru
× Iwamori, Hikaru |
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| 著者別名 | ||||||
| 識別子Scheme | WEKO | |||||
| 識別子 | 126193 | |||||
| 姓名 | 岩森, 光 | |||||
| 著者所属 | ||||||
| 著者所属 | Department of Earth and Planetary Sciences, University of Tokyo | |||||
| 抄録 | ||||||
| 内容記述タイプ | Abstract | |||||
| 内容記述 | Recent knowledge concerning the phase relationships of hydrous peridotitic and basaltic systems allows us to model fluid generation and migration in subduction zones. Here I present: (1) numerical models for the transportation of H2O and melting beneath the Japanese islands, in which generation and migration of aqueous fluid, its interaction with the convecting solid, and melting are considered, based on the phase relationships; (2) predictions of the corresponding seismic structures based on the calculated distribution of the fluids (aqueous fluids and melts); (3) 3-D seismic tomographic images beneath the islands; (4) analyses of the distribution of the volcanoes and the volcanic chains; and (5) comparisons between the model predictions and the observations. The model calculation suggests that in northeast Japan, nearly all of the H2O expelled from the subducted Pacific plate is hosted by serpentine and chlorite just above the plate, and is brought down to～150 km. Breakdown of serpentine and chlorite at these depths results in the formation of a fluid column through which H2O is transported upwards, and results in the initiation of melting in the mantle wedge beneath the backarc. Seismic tomographic studies suggest the existence of such a melting region beneath the backarc. In central Japan, the subducted Philippine Sea plate overlaps the subducted Pacific plate. This geometry causes slow thermal recovery of the subducted Pacific plate, resulting in dehydration reactions at levels (200-300 km) deeper than in northeast Japan, and deflection of the volcanic chain towards the backarc side. In contrast, in southwest Japan, where a relatively hot part of the Philippine sea plate (Shikoku basin) subducts, the dehydration reactions are predicted to occur at relatively shallow levels (< 100 km in depth). The seismic tomographic image supports well the predicted distribution of the fluids beneath the volcanic front to the forearc region. These comparisons between the model predictions and the observations suggest that the thermal structure (determined by age and subduction velocity) of the subducting plate strongly controls the distribution of the aqueous fluids and melts in subduction zones through the position of the dehydration reactions. | |||||
| 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. 377-389, 発行日 2002-02-12 |
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| 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 | ||||||
