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作 者:黄永海[1] HUANG Yong-hai(Anhui Institute of geological survey,Hefei 230001,China)
出 处:《世界有色金属》2018年第15期68-68,70,共2页World Nonferrous Metals
摘 要:长龙山位于繁昌县荻港镇东部,桃冲铁矿西部。地处长江中下游成矿带中间地段。通过一系列普查工作,在古家冲一带中浅部,有寻找矽卡岩型铜铅锌多金属矿的前景,深部有找寻矽卡岩型铁矿(磁铁矿、赤铁矿、镜铁矿)的可能。板子矶水泥厂附近具有找寻磁铁矿的前景。在荻港体育场东部具有寻找裂隙型金矿的前景。The longlongshan is located in the eastern part of the town of Di Gang,Fanchang County,west of the peach Chong iron mine.It is located in the middle part of the middle and lower reaches of the Yangtze River metallogenic belt.Through a series of surveys,it is possible to find skarn type copper-lead-zinc polymetallic deposits in the middle and shallow parts of Gujiachong area,and skarn type iron deposits(magnetite,hematite and specularite)in the deep part.There is a prospect for magnetite in the vicinity of the pan Ji cement plant.In the east of the di Kong Stadium,there is a prospect for finding fractured gold deposits.
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