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guang dong wu hua xian qing gang qian xin kuang qu di zhi te zheng ji cheng yin chu tan
Author(s): 
Pages: 4-6
Year: Issue:  2
Journal: XINJIANG YOUSE JINSHU

Abstract: 青岗铅锌矿主要产于下侏罗统金鸡组地层的断裂构造(F1)破碎角砾岩带中,矿体产出的形态和空间分布受导矿构造引发的围岩裂隙形态控制,矿体呈透镜状、脉状,倾向169°~180°,倾角45°~56°,个别63° 以上矿体在地表露头表现为黄铁、褐铁矿化脉;显微镜镜下矿物特征和矿物组合特点等表明,该矿床类型属多期次成矿活动的中低温热液充填交代型矿床.
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