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昭和基地周辺に産するEvaporiteならびに黄色塩類の鉱物組成
https://doi.org/10.15094/00007531
https://doi.org/10.15094/00007531197eeb2c-e730-4528-818b-9fb9acb6fd60
名前 / ファイル | ライセンス | アクション |
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KJ00002476453 (4.2 MB)
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Item type | 紀要論文(ELS) / Departmental Bulletin Paper(1) | |||||
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公開日 | 1968-12-01 | |||||
タイトル | ||||||
タイトル | 昭和基地周辺に産するEvaporiteならびに黄色塩類の鉱物組成 | |||||
タイトル | ||||||
言語 | en | |||||
タイトル | MINERALOGICAL COMPOSITION OF WHITE EVAPORITES AND YELLOW SALTS FOUND AROUND SYOWA STATION, ANTARCTICA | |||||
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 | 10.15094/00007531 | |||||
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 | ショウワキチ シュウヘン ニ サンスル Evaporite ナラビニ オウショク エンルイ ノ コウブツ ソセイ | |||||
著者名(日) |
兼島, 清
× 兼島, 清× 鳥居, 鉄也× 宮平, 勝昭 |
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著者名(英) |
KANESHIMA, Kiyoshi
× KANESHIMA, Kiyoshi× TORII, Tetsuya× MIYAHIRA, Katsuaki |
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著者所属(日) | ||||||
琉球大学理工学部 | ||||||
著者所属(日) | ||||||
千葉工業大学 | ||||||
著者所属(日) | ||||||
琉球大学理工学部 | ||||||
著者所属(英) | ||||||
en | ||||||
Faculty of Science, University of the Ryukyus | ||||||
著者所属(英) | ||||||
en | ||||||
Chiba Institute of Technology | ||||||
著者所属(英) | ||||||
en | ||||||
Faculty of Science, University of the Ryukyus | ||||||
抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | During the summer mission of the 8th Japanese Antarctic Research Expedition (1966-1967), white evapontes and yellow salts were collected around Syowa Station, and their chemical and mmeralogical characteristics were studied. Eleven species of the white evapontes and eight species of the yellow salts were analyzed chemically, and mmeralogical components were identified by X-ray diffraction method. The white evapontes can be grouped into six types by the mmeralogical components as follows. (1) Halite, Sylvite, (L-1, L-2) (2) Halite, Sylvite, Bloedite (E-1, E-2, E-4) (3) Halite, Sylvite, Bloedite, Epsomite (E-5, E-13) (4) Halite, Sylvite, Bloedite, Thenardite (E-6, E-16) (5) Halite, Thenardite, Mirabihte, Bloedite, Gypsum (E-10, E-12) (6) Gypsum, Halite, Thenardite (E-15) The characteristics of the white evaporites found around Syowa Station are as follows. (1) Main component is halite. (2) Magnesium compounds are contained as epsomite or bloedite. (3) The presence of thenardite, mirabilite and gypsum is observed. (4) The white evapontes cannot be grouped by the mode of occurrence. The results of the X-ray diffraction analysis show that the yellow salts consist of gypsum, iron hydroxy sulf ate (carphosidente and copiapite), and halite. The yellow salts can be grouped into two types by the mineralogical components as follows (1) Gypsum, Garphosidente, Halite (E-8, E-14-B, E-9, E-14-A) (2) Gypsum, Carphosiderite, Copiapite Halite (E-7, E-14-G) To discuss the formation of yellow salts, samples of the soft yellowish brown weathered rock and hard quartzy rock were analyzed, and the dissolution experiments were also carried out. | |||||
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 33, p. 39-52, 発行日 1968-12 |
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出版者 | ||||||
出版者 | 国立極地研究所 |