Abstract
The marcasite-native sulphur deposit of the Kusu mine is shallow seated epithermal replacement type and the ore forming agent may have been an acending hydrothermal sulphuric solution of volcanic origin. The mother rock alteration of the Kusu mine are described in detail. They are characterzed by the Tonal arrangement of wall rock alteration such as silica rock, kaolinite clay, ore body, kaolinite clay and original rock from the surface to down ward.
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Schedule a callMore From: The Journal of the Japanese Association of Mineralogists, Petrologists and Economic Geologists
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