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The crystal structure of scapolite in the Luetzow-Holm Bay region, East Antarctica
https://doi.org/10.15094/00003090
https://doi.org/10.15094/000030901139100d-0372-4447-8dfd-f849edb95c17
名前 / ファイル | ライセンス | アクション |
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KJ00000044208 (1.9 MB)
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Item type | 紀要論文(ELS) / Departmental Bulletin Paper(1) | |||||
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公開日 | 2001-10-01 | |||||
タイトル | ||||||
タイトル | The crystal structure of scapolite in the Luetzow-Holm Bay region, East Antarctica | |||||
言語 | ||||||
言語 | eng | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | scapolite | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | meionite | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | marialite | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | crystal structure | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | East Antarctica | |||||
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 | 10.15094/00003090 | |||||
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 | The crystal structure of scapolite in the Luetzow-Holm Bay region, East Antarctica | |||||
著者名(英) |
Yamakawa,Junji
× Yamakawa,Junji× Ando,Yumi× Osanai,Yasuhito× Kusachi,Isao |
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著者所属(英) | ||||||
en | ||||||
Department of Earth Sciences, Faculty of Science, Okayama University/Graduate School of Social and Cultural Studies, Kyushu University/Department of Earth Sciences, Faculty of Education, Okayama University/Department of Earth Sciences, Faculty of Education, Okayama University | ||||||
抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | The crystal structure of scapolite from the Liitzow-Holm Bay region, East Antarctica with cell formular (Na_<1.97>Ca_<1.48>K_<0.46>Mg_<0.03>) _<3.94> (Al_<4.15>Si_<7.85>Fe_<0.01>) _<12.01>O_<24.00> (Cl_<0.65>(CO_3) _<0.42>) _<1.07>, Me_<39>, was determined in tetragonal, P4_2/n, a=12.122(2); c=7.585(2) A by the single crystal X-ray diffraction method. The structure is the same as that of meionite but with some difference in atomic coordinates and Al percentage in the tetrahedon. The CO_3 groups were mainly disordered on the xy plane and off-centred from the Anion site. The cation site was 8-coordinate rather than 6-coordinate. | |||||
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 14, p. 139-156, 発行日 2001-10 |
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出版者 | ||||||
出版者 | National Institute of Polar Research |