Mineralization styles are dominantly veinlet-disseminated and veinlet, occasionally stockwork.
铜、金矿化主要呈细脉浸染状和细脉状，偶见网脉状。
Mineralization styles are dominantly veinlet-disseminated and veinlet, occasionally stockwork.
铜、金矿化主要呈细脉浸染状和细脉状，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...
矿化亦相应具有分带性,从蚀
中心向外表现为浸染状黄铜矿、辉钼矿→细脉浸染状黄铁矿、黄铜矿→细脉状黄铁矿、黄铜矿→大脉状方铅矿、黄铁矿。
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