岩石鉱物鉱床学会誌
Online ISSN : 1883-0765
Print ISSN : 0021-4825
ISSN-L : 0021-4825
阿蘇中央火口丘火山岩中の銅含有量
松本 幡郎小沢 竹二郎
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1967 年 58 巻 6 号 p. 213-217

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The Cu contents of twenty five representative rock samples from the central cones of Aso volcano have been determined by the Sandell's colorimetric method. They range from 0.001 to 0.015 per cent and generally tend to be higher in basic rocks and lower in acidic ones. It has been also noticed that the rock types produced by fractional crystallization of high-alumina basalt magma have higher Cu contents, while those formed by contamination have lower.

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