广西贵港市龙头山铜矿特征及找矿标志
Yunnan Geology（2020）
Abstract
广西贵港市龙头山铜矿为隐伏矿,矿体产状呈脉状、透镜状赋存于龙头山侵入岩-次火山岩体及周边围岩构造裂隙中,铜矿的形成与本地区燕山期岩浆侵入活动关系密切,属燕山晚期岩浆热液型矿床.在400m标高以下的,且具有明显的黄铁矿化岩体接触构造带是主要的找矿标志.
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