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東オングル島産柘榴石について(地学部門)(<特集>南極シンポジウム)
https://doi.org/10.15094/00007009
https://doi.org/10.15094/000070091cabe536-4334-455c-9927-65e9094a7f88
名前 / ファイル | ライセンス | アクション |
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KJ00002406673 (1.2 MB)
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Item type | 紀要論文(ELS) / Departmental Bulletin Paper(1) | |||||
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公開日 | 1961-01-01 | |||||
タイトル | ||||||
タイトル | 東オングル島産柘榴石について(地学部門)(<特集>南極シンポジウム) | |||||
タイトル | ||||||
言語 | en | |||||
タイトル | Garnet from East Ongul Island in the Antarctic Region (EARTH SCIENCE) (<Special Publication>Antarctic Symposium in Tokyo, 1960) | |||||
言語 | ||||||
言語 | jpn | |||||
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 | 10.15094/00007009 | |||||
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 | ヒガシ オングルトウ サン ザクロイシ ニ ツイテ | |||||
著者名(日) |
南, 英一
× 南, 英一× 小坂, 丈予× 中村, 忠晴 |
|||||
著者名(英) |
MINAMI, Eiichi
× MINAMI, Eiichi× OSSAKA, Joyo× NAKAMURA, Tadaharu |
|||||
著者所属(日) | ||||||
上智大学 | ||||||
著者所属(日) | ||||||
東京大学地震研究所 | ||||||
著者所属(日) | ||||||
早稲田大学第一理工学部 | ||||||
著者所属(英) | ||||||
en | ||||||
Sophia University | ||||||
著者所属(英) | ||||||
en | ||||||
Earthquake Research Institute, University of Tokyo | ||||||
著者所属(英) | ||||||
en | ||||||
Waseda University | ||||||
抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | The sample was collected by Prof. Torii of Chiba University. Its colour is reddish brown and translucent and it forms a somewhat elongated crystal. It shows a few cracks and is brittle. Observed under the microscope, the greater part of the thin sections is quite homogeneous, but the bottom part of the crystal contains very small amount of hornblende, limonite and albite. We select its homogeneous part for our study. The following result were obtained: S.G. 3.954±0.005 a_0 11.530 Å (lattice constant) nNa 1.778±0.002 Si0_2 40.02% Al_20_3 21.90 Fe_20_3 1.53 FeO 21.34 CaO 5.20 MgO 8.94 K_20 0.01 Na_20 0.06 H_20^- 0.18 H_20^+ - Ti0_2 0.06 P_20_5 0.00 MnO 0.93 SrO 0.00 Total 100.17% F 0.002% Less 0 for F: 0.001% Rb and Li were detected by spectrochemical analysis, but Cr was not detected and, therefore, uvarovite-component is absent. Other rarer elements were not found. From the result of chemical analysis the authors studied its garnet-components and obtained the following results: Almandite 47.64% Andradite 4.59% Pyrope 35.49% Grossularite 10.10% Spessartite 2.18% By Boeke's classification this constitution belongs to pyralspite. | |||||
雑誌書誌ID | ||||||
収録物識別子タイプ | NCID | |||||
収録物識別子 | AN00181831 | |||||
ISSN | ||||||
収録物識別子タイプ | ISSN | |||||
収録物識別子 | 00857289 | |||||
書誌情報 |
南極資料 巻 11, p. 751-755, 発行日 1961-01 |
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国際十進分類法 | ||||||
主題Scheme | UDC | |||||
主題 | 551.1/.4:552 | |||||
出版者 | ||||||
出版者 | 国立極地研究所 |