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铜陵矿集区茗山岩体地质特征与找矿前景探讨
引用本文:马晓红.铜陵矿集区茗山岩体地质特征与找矿前景探讨[J].安徽地质,2011(4):247-251.
作者姓名:马晓红
作者单位:安徽省地质实验研究所,安徽合肥230001
摘    要:位于铜陵矿集区南部的茗山石英二长闪长岩是本区"五通组"以下早古生代地层中开展"第二成矿空间"找矿的"窗口",本文通过对该岩体地球化学研究表明,其主要特征与铜陵地区成矿岩体地球化学特征相同,应是矿集区岩浆成矿系统的一部分,进一步开展岩体含矿性及其深部与早古生代碳酸盐岩地层接触带部位的矿产勘查对于指导铜陵矿集区的深部找矿具有重要意义。

关 键 词:茗山岩体  地球化学  部找矿  铜陵矿集区

GEOLOGICAL FEATURES OF THE MINGSHAN INTRUSION IN THE TONGLING MINING CAMP AND ORE-PROSPECTING OUTLOOK
MA Xiao-hong.GEOLOGICAL FEATURES OF THE MINGSHAN INTRUSION IN THE TONGLING MINING CAMP AND ORE-PROSPECTING OUTLOOK[J].Geology of Anhui,2011(4):247-251.
Authors:MA Xiao-hong
Institution:MA Xiao-hong(Institute of Geoanalysis of Anhui Province,Hefei,Anhui 230001,China)
Abstract:The Mingshan quartz monzodiorote in the Tongling mining camp is ore-prospecting "window" in early Paleozoic strata underlying the "Wutong Formation" in the area.Geochemical study of the intrusion indicates that its major features are the same with those of mineralized ore bodies in the Tongling area,and this intrusion should be a part of the magmatic mineralizing system in the mining camp,and further study of ore potential in the intrusion and mineral exploration in the depth and in the contact with early Paleozoic carbonatite are significant to guiding ore prospecting in the depth in the Tongling mining camp.
Keywords:the Mingshan intrusion  geochemistry  deep ore prospecting  the Tongling mining camp
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