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高圧・超高圧変成岩のフェンジャイト年代学 : 故鈴木和博氏に捧ぐ
https://doi.org/10.18999/nagubc.1.11
https://doi.org/10.18999/nagubc.1.1156bae54e-7c84-4e95-a711-fbe9c6edda7b
名前 / ファイル | ライセンス | アクション |
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Item type | 紀要論文 / Departmental Bulletin Paper(1) | |||||
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公開日 | 2018-08-17 | |||||
タイトル | ||||||
タイトル | 高圧・超高圧変成岩のフェンジャイト年代学 : 故鈴木和博氏に捧ぐ | |||||
言語 | ja | |||||
その他のタイトル | ||||||
その他のタイトル | Phengite geochronology of HP-UHP metamorphic rocks : to the late Kazuhiro Suzuki | |||||
言語 | en | |||||
著者 |
板谷, 徹丸
× 板谷, 徹丸× Itaya, Tetsumaru |
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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 | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | HP-UHP metamorphic rocks | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | phengite | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | K-Ar geochronology | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | fast and slow schists | |||||
抄録 | ||||||
内容記述 | This review is dedicated to the memory of the late Kazuhiro Suzuki, a professor emeritus of Nagoya University who passed away on October 15, 2016. Kazuhiro Suzuki was the most important member of the Japan Geochronology Network (jGnet), and the main contributor to the development of jGnet. This paper seeks to accomplish two things: first, to introduce the author’s evaluation of the CHIME method conceived by Kazuhiro Suzuki; second, to report on the phengite geochronology of HP-UHP metamorphic rocks the author has been studying for 30 years. Phengite undergoes dynamic recrystallization during the deformation of rocks in the exhumation. Ar is released from the phengite crystals during the process, as documented in the in-situ Ar-Ar dating of phengites with equant shapes included in rigid garnet and of stretched phengites in the matrix. The duration of deformation during the exhumation after the peak metamorphism shows the average values from the peak metamorphism to the deformation ceasing level, making it possible to calculate the exhumation rates. A high exhumation (strain) rate makes a “fast schist” sequence consisting of several units whose boundaries are distinct faults. A low exhumation (strain) rate makes a “slow schist” sequence with a large-scale recumbent fold. | |||||
言語 | en | |||||
内容記述タイプ | Abstract | |||||
出版者 | ||||||
言語 | ja | |||||
出版者 | 名古屋大学宇宙地球環境研究所年代測定研究部 | |||||
言語 | ||||||
言語 | jpn | |||||
資源タイプ | ||||||
資源 | http://purl.org/coar/resource_type/c_6501 | |||||
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 | 10.18999/nagubc.1.11 | |||||
ID登録タイプ | JaLC | |||||
書誌情報 |
ja : 名古屋大学年代測定研究 巻 1, p. 11-22, 発行日 2017-03-31 |
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著者版フラグ | ||||||
値 | publisher |