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浅谈岿美山钨矿成矿规律及找矿方向
引用本文:李常青.浅谈岿美山钨矿成矿规律及找矿方向[J].矿产与地质,2010,24(2):136-140.
作者姓名:李常青
作者单位:江西岿美山钨业有限公司,江西,定南,341902
摘    要:岿美山钨矿包括西部含黑钨石英脉组及南部矽卡岩白钨矿体,探矿均未超过500m标高以下范围;经过几十年的生产实践和对深、边部的勘探,认为石英脉型黑钨矿向南西方向侧伏明显,内接触带中有大量石英脉,且有不同程度矿化,有二次成矿的条件,砂包常见。指出矿区西部及北东、南东方向有找矿潜力。

关 键 词:钨矿  内接触成矿  二次成矿  砂包  岿美山  江西

Discussion on metallogenic regularity and exploration direction of Guimeishan tungsten deposit
LI Chang-qing.Discussion on metallogenic regularity and exploration direction of Guimeishan tungsten deposit[J].Mineral Resources and Geology,2010,24(2):136-140.
Authors:LI Chang-qing
Institution:LI Chang-qing(Jiangxi Guimeishan Tungsten Industry Co.,Ltd.,Dingnan,Jiangxi 341902)
Abstract:Guimeishan tungsten deposit includes wolframite quartz vein group in the west and skarn scheelite orebody in the south. The exploration depth is not below 500 meters level. For the production practice and exploration in the depth and border of the mine in the past several decades,it is proposed that wolframite quartz vein is lateral trending towards southwest obviously. There are a lots of quartz veins in the inner contact zone with mineralization of different degree. The secondary mineralization condition is good. There are some ore wraps to be often found. The paper has pointed out the prospecting potential in the west,northeast and southeast direction of the mine.
Keywords:tungsten deposit  inner contact mineralization  secondary mineralization  ore wrap  Guimeishan  Jiangxi
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