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,从蚀变中心向外表现为染状黄铜矿、辉钼矿→细脉染状黄铁矿、黄铜矿→细脉状黄铁矿、黄铜矿→大脉状方铅矿、黄铁矿。
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,从蚀变中心向外表现为染状黄铜矿、辉钼矿→细脉染状黄铁矿、黄铜矿→细脉状黄铁矿、黄铜矿→大脉状方铅矿、黄铁矿。
Abstract: The Zhaiwa Mo deposit in the Xiong’er Mountain of western Henan Province is a quartz veintype molybdenite deposit newly discovered in the hypometamorphic rocks of Archean Taihua Group.
中文摘要: 寨凹钼矿床位于河南地区,是新发现的穿插于太古宙太华岩群深变质岩中的辉钼矿石英脉型钼矿床。
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