Mineralization styles are dominantly veinlet-disseminated and veinlet, occasionally stockwork.
铜、金矿化主要呈脉浸脉,偶见网脉。
Mineralization styles are dominantly veinlet-disseminated and veinlet, occasionally stockwork.
铜、金矿化主要呈脉浸脉,偶见网脉。
The metallogenesis is zoned correspondingly.There are disseminated chalcopyrite,molybdenite→veinlet disseminated pyrite,chalcopyrite→veinlet pyrite,chalcopyrite→vein galenite,pyr...
矿化亦相应具有分带性,从蚀中心向外表现为浸铜矿、辉钼矿→脉浸铁矿、铜矿→脉铁矿、铜矿→大脉方铅矿、铁矿。
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