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A cooling rate constraint on microtextural development of plagioclase and scapolite: an example from the Lutzow-Holm Complex, East Antarctica
https://doi.org/10.15094/00003124
https://doi.org/10.15094/00003124d2cee6cb-de8b-491f-ad00-34ba81d016cb
名前 / ファイル | ライセンス | アクション |
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KJ00000044118 (1.4 MB)
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Item type | 紀要論文(ELS) / Departmental Bulletin Paper(1) | |||||
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公開日 | 2003-10-01 | |||||
タイトル | ||||||
タイトル | A cooling rate constraint on microtextural development of plagioclase and scapolite: an example from the Lutzow-Holm Complex, East Antarctica | |||||
言語 | ||||||
言語 | eng | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | cooling rate | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | exhumation rate | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | Lutzow-Holm Complex | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | microtexture | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | transmission electron microscope analysis | |||||
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 | 10.15094/00003124 | |||||
ID登録タイプ | JaLC | |||||
ページ属性 | ||||||
内容記述タイプ | Other | |||||
内容記述 | P(論文) | |||||
著者名(英) |
Miyake, Akira
× Miyake, Akira× Seto, Yusuke× Kitamura, Masao |
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著者所属(英) | ||||||
en | ||||||
Department of Geology and Mineralogy, Graduate School of Science, Kyoto University | ||||||
著者所属(英) | ||||||
en | ||||||
Department of Geology and Mineralogy, Graduate School of Science, Kyoto University | ||||||
著者所属(英) | ||||||
en | ||||||
Department of Geology and Mineralogy, Graduate School of Science, Kyoto University | ||||||
抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | Exsolution lamellae in albite-rich plagioclase and antiphase domains in scapolite from the Lutzow-Holm Complex of East Antarctica were found under a transmission electron microscope.These micro-textures were found in the first cooling period of the three period cooling model proposed from the geochronological data. Based on these micro-textures,the cooling rate of the complex was estimated to be in a range from several to thousands K/my. These rates are concordant with those estimated from the ages of the complex. | |||||
雑誌書誌ID | ||||||
収録物識別子タイプ | NCID | |||||
収録物識別子 | AA1130866X | |||||
書誌情報 |
Polar geoscience 巻 16, p. 100-107, 発行日 2003-10 |
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出版者 | ||||||
出版者 | National Institute of Polar Research |