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MICROSTRUCTURE OF PERTHITES IN SYENITES FROM THE YAMATO MOUNTAINS, EAST ANTARCTICA
https://doi.org/10.15094/00002849
https://doi.org/10.15094/000028490b756884-746f-4f0e-bc89-838c4f668665
名前 / ファイル | ライセンス | アクション |
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KJ00002368122 (974.4 kB)
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Item type | 紀要論文(ELS) / Departmental Bulletin Paper(1) | |||||
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公開日 | 1997-09-01 | |||||
タイトル | ||||||
タイトル | MICROSTRUCTURE OF PERTHITES IN SYENITES FROM THE YAMATO MOUNTAINS, EAST ANTARCTICA | |||||
言語 | ||||||
言語 | eng | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | Albite-twin | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | alkali feldspar | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | cryptoperthite | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | K-feldspar | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | perthite | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | syenite | |||||
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 | 10.15094/00002849 | |||||
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) | |||||
論文名よみ | ||||||
その他のタイトル | MICROSTRUCTURE OF PERTHITES IN SYENITES FROM THE YAMATO MOUNTAINS, EAST ANTARCTICA | |||||
著者名よみ |
オオバ, タカノブ
× オオバ, タカノブ× ウエハラ, セイイチロウ× シライシ, カズユキ |
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著者名(英) |
OBA, Takanobu
× OBA, Takanobu× UEHARA, Seiichirou× SHIRAISHI, Kazuyuki |
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著者所属(英) | ||||||
en | ||||||
Department of Geoscience, Joetsu University of Education | ||||||
著者所属(英) | ||||||
en | ||||||
Department of Earth and Planetary Sciences, Kyushu University | ||||||
著者所属(英) | ||||||
en | ||||||
National Institute of Polar Research | ||||||
抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | Cryptoperthites in intrusive syenite from the Yamato Mountains were studied by transmission electron microscopy. They consist of two domains, one being narrow Albite-twinned plagioclase, the other a triclinic K-feldspar. The crystal symmetry of the majority of K-feldspars from the Yamato Mountains is triclinic; while monoclinic symmetry is rare. The triclinicity of K-feldspar ranges from 0.34 to 0.59. There is no difference in triclinicity between K-feldspar from the northern and southern Yamato Mountains. The exsolution lamelae do not develop a zig-zag pattern in either area. This fact suggests that the cooling rate of intrusive syenites from the Yamato Mountains is not very slow. Plagioclase in myrmekite, perthite and antiperthite in syenite from the southern Yamato Mountains is oligoclase (An_<19.6>Ab_<79.7>Or_<0.7>∿An_<14.9>Ab_<68.9>Or_<16.2>) with low Or content, whereas plagioclase of composition An_<0.3>Ab_<99>Or_<0.7>∿An_<0.3>Ab_<82>Or_<17.7> occurs as patches and wavy strings in perthite from the northern area. Although plagioclase is more anorthitic in syenite from the south than from the north, the chemical composition of K-feldspar is similar in both areas. | |||||
雑誌書誌ID | ||||||
収録物識別子タイプ | NCID | |||||
収録物識別子 | AA1072335X | |||||
書誌情報 |
Proceedings of the NIPR Symposium on Antarctic Geosciences 巻 10, p. 120-129, 発行日 1997-09 |
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出版者 | ||||||
出版者 | National Institute of Polar Research |