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内蒙古吉林宝力格银矿床地质特征及找矿标志
引用本文:江和中,刘国范,刘伟芳.内蒙古吉林宝力格银矿床地质特征及找矿标志[J].华南地质与矿产,2007(4):9-13.
作者姓名:江和中  刘国范  刘伟芳
作者单位:河南省第一地质勘查院,河南,南阳473003
摘    要:在研究矿床地质特征的基础上,认为内蒙古吉林宝力格银矿床是火山喷流沉积-燕山早期岩浆热液叠加改造块状硫化物多金属矿床。区域上EW向古生代形成的裂谷型上泥盆统-下二迭的浅变质沉积-火山岩系,是本区找矿的最佳区段。含银流纹质晶屑凝灰岩是银多金属矿的重要找矿标志。

关 键 词:银矿床  火山喷流沉积  热液叠加改造  找矿标志  内蒙古吉林宝力格
文章编号:1007-3701(2007)04-0009-05
收稿时间:2007-06-30
修稿时间:2007年6月30日

Geological Characteristics and Mineral Resource Prospecting of Jilinbaolige Silver Deposit, Inner Mongolia
JIANG He-zhong,LIU Guo-fan,LIU Wei-fang.Geological Characteristics and Mineral Resource Prospecting of Jilinbaolige Silver Deposit, Inner Mongolia[J].Geology and Mineral Resources of South China,2007(4):9-13.
Authors:JIANG He-zhong  LIU Guo-fan  LIU Wei-fang
Abstract:Based on studies on geological character of the deposit,it is an early stage volcanic projection-deposition of Yanshanian magmatism and the massive sulfide polymetllic deposit which is reformed by hydrothermal fluid.Regional E-W direction rift type epizonal metamorphic-volcanic formation of upper Devonian and low Permian series is available sector for prospecting in the area.Bearing-silver rhyolitic crystal tuff is the important criteria for ore prospecting in the silver polymetllic deposit.
Keywords:silver deposit  volcanic-projection-deposit  hydrothermal reformed  criteria for ore prospecting  Jilinbaolige  Inner Mongolia
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