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
,
蚀变中心向外表现为
状黄铜矿、辉钼矿→细
状黄铁矿、黄铜矿→细状黄铁矿、黄铜矿→大状方铅矿、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,蚀变中心向外表现为状黄铜矿、辉钼矿→细状黄铁矿、黄铜矿→细状黄铁矿、黄铜矿→大状方铅矿、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熊耳山地区，是新近发现的穿插于太古宙太华岩群深变质岩中的辉钼矿石英型钼矿床。
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