Item type |
紀要論文(ELS) / Departmental Bulletin Paper(1) |
公開日 |
2003-10-01 |
タイトル |
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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 |
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言語 |
eng |
キーワード |
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主題Scheme |
Other |
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主題 |
cooling rate |
キーワード |
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主題Scheme |
Other |
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主題 |
exhumation rate |
キーワード |
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主題Scheme |
Other |
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主題 |
Lutzow-Holm Complex |
キーワード |
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主題Scheme |
Other |
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主題 |
microtexture |
キーワード |
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主題Scheme |
Other |
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主題 |
transmission electron microscope analysis |
資源タイプ |
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資源タイプ識別子 |
http://purl.org/coar/resource_type/c_6501 |
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資源タイプ |
departmental bulletin paper |
ID登録 |
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ID登録 |
10.15094/00003124 |
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ID登録タイプ |
JaLC |
ページ属性 |
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内容記述タイプ |
Other |
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内容記述 |
P(論文) |
著者名(英) |
Miyake, Akira
Seto, Yusuke
Kitamura, Masao
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著者所属(英) |
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en |
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Department of Geology and Mineralogy, Graduate School of Science, Kyoto University |
著者所属(英) |
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en |
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Department of Geology and Mineralogy, Graduate School of Science, Kyoto University |
著者所属(英) |
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en |
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Department of Geology and Mineralogy, Graduate School of Science, Kyoto University |
抄録(英) |
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内容記述タイプ |
Other |
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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 |
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収録物識別子タイプ |
NCID |
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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 |
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出版者 |
National Institute of Polar Research |