Geochemical Investigations of Minerals in the Antarctic
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概要
- 論文の詳細を見る
Many evaporites, such as halite, sylvite, epsomite, mirabilite, bloedite, gypsum, carphosiderite, aragonite, hexahydrite and atakamite were found around Syowa Station. These minerals are thought to have been formed by sea spray and/or concentration under the frigid condition, and in some cases by rock weathering. Garnet and euxenite were analyzed from the view points of geochemistry and mineralogy. On the other hand, a new mineral, antarcticite, was found by geochemical investigation in the Dry Valleys. In the Dry Valley Drilling Project, many evaporites and secondary minerals were analyzed by X-ray and chemical method, and from these results the geological processes in the Dry Valley were clarified to some extent.
- 国立極地研究所の論文
著者
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Torii Tetsuya
Chiba Institute of Technology
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Watanuki Kunihiko
Department Of Chemistory The College Of Arts And Sciences The University Of Tokyo
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Watanuki Kunihiko
Department Of Chemistry College Of General Education University Of Tokyo
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Morikawa Hideki
Research Laboratory Of Engineering Material Tokyo Institute Of Technology
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Nishiyama Takashi
Department Of Applied Chemistry Graduate School Of Engineering Tokyo University Of Agriculture And T
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Nishiyama Takashi
Department of Aeronautics and Astronautics, Faculty of Engineering, Kyushu University, Motooka, Nishi-ku, Fukuoka 819-0395, Japan
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NISHIYAMA Takashi
Department of Aeronautics and Astronautics, Faculty of Engineering, Kyushu University
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