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作 者:王珍 陈立泉 WANG Zhen;CHEN Li-quan(The Sixth Geological Brigade of Jiangxi Geological Bureau,Yingtan 335001,China)
机构地区:[1]江西省地质局第六地质大队,江西鹰潭335001
出 处:《世界有色金属》2024年第21期34-36,共3页World Nonferrous Metals
摘 要:横山铜多金属矿位于铅山县永平铜矿的西部外围,为实现对横山地区找矿突破,在横山地区采用路线地质调查、1/1万土壤地球化学测量、广域电磁测深测量等地质手段,发现横山出露的构造角砾岩带中铁帽含硫化物发育。经对横山地区物化探特征进行了综合分析,结果表明物化探特征与地表矿化特征相吻合,横山地区深部可能赋存铜多金属矿(化)体,找矿潜力较大。The Hengshan Copper Polymetallic Mine is located on the western periphery of the Yongping Copper Mine in Qianshan County.In order to achieve a breakthrough in mineral exploration in the Hengshan area,geological methods such as route geological survey,1/10000 soil geochemical measurement,and wide area electromagnetic depth measurement were used to discover the development of iron cap sulfide in the exposed tectonic breccia belt in Hengshan.After comprehensive analysis of the physical and chemical exploration characteristics in Hengshan area,the results show that the characteristics of physical and chemical exploration are consistent with the surface mineralization characteristics.There may be copper polymetallic ore(mineralization)bodies in the deep part of Hengshan area,which has great potential for mineral exploration.
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