湖南茶盘元铜铅矿地质特征及找矿前景分析

Geological characteristics and prospecting analysis of Chapanyuan copper-lead deposit in Hunan

湖南茶盘元铜铅矿位于塔山岩体北西侧接触带,已知矿脉赋存于北东向断裂中.通过分析矿床成矿地质条件及矿床地质特征,推断该矿床为与岩浆岩有关的低温热液裂隙充填型矿床;该矿床找矿标志明显,有扩大矿床规模的找矿前景,深部是寻找高温热液型金属矿床的有利地段.

Hunan Chapanyuan Copper-Lead Mine is located in the contact zone on the northwest side of the Tashan rock mass,It is known that the ore veins occur in the NE fault.By analyzing the ore-forming geological conditions and geological characteristics of the deposit,It is inferred that the deposit is a low-temperature hydrothermal fissure-filling deposit related to magmatic rocks;The prospecting sign of this deposit is obvious,and there is prospect for prospecting to expand the scale of the deposit,The deep part is a favorable area for finding high temperature hydrothermal metal deposits.