Mineralization styles are dominantly veinlet-disseminated and veinlet, occasionally stockwork.
铜、金化主要呈脉浸染状和脉状,偶见网脉状。
Mineralization styles are dominantly veinlet-disseminated and veinlet, occasionally stockwork.
铜、金化主要呈脉浸染状和脉状,偶见网脉状。
The metallogenesis is zoned correspondingly.There are disseminated chalcopyrite,molybdenite→veinlet disseminated pyrite,chalcopyrite→veinlet pyrite,chalcopyrite→vein galenite,pyr...
化亦相应具有分带性,从蚀中心向外表现为浸染状黄铜、辉钼→脉浸染状黄、黄铜→脉状黄、黄铜→大脉状方铅、黄。
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