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Orientation Analysis and Formation Ages of Fractures Filled with Clay Minerals (Clay Veins) in Hiroshima and Shimane Prefectures, Southwest Japan
1994
Journal of the Japan Society of Engineering Geology
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Fractures filled with clay minerals (clay veins) occur extensively in granitic andrhyolitic rocks throughout Hiroshima and Shimane Prefectures, southwest Japan. The main constituent clay minerals are mica clay mineral,
doi:10.5110/jjseg.35.60
fatcat:mydmgzisonbprkitquezqafmbe