安徽省枞阳县柳峰山地区金铜矿点地质特征及找矿方向  

Geological features of gold-copper prospects and the exploration direction in the Liufengshan area, Zongyang County, Anhui Province

作　　者：姚成侯 王亚光 

机构地区：[1]安徽省昌华矿业有限公司,安徽合肥230000

出　　处：《安徽地质》2012年第3期183-185,共3页Geology of Anhui

摘　　要：安徽省枞阳县柳峰山地区金铜矿是热液充填形成的脉状矿床。矿体严格受断裂带控制、矿脉的力学性质以扭压性为主、矿脉铜金矿与岩脉关系极为密切、主要的铜金矿脉均有岩脉相伴。火山口的外围断裂构造中,岩脉的发育的地区,断裂构造的交汇部位是今后找矿的重点部位。The gold-copper prospects are vein deposits formed by hydrothermal filling in the Liufengshan area,Zongyang County,Anhui Province.Ore bodies are precisely controlled by fault zone,vein mechanics is dominantly shearing compressive,vein gold and copper are closely related to dykes,and all major copper and gold veins are associated with dykes.The key exploration areas are in the peripheral rifted structures of volcanic vent,where dykes are well developed,and rifted structures meet.

关 键 词：热液充填的脉状矿床 岩脉 火山口的外围断裂构造 找矿方向 

分 类 号：P618.41[天文地球—矿床学]