辽宁青城子地区金、银矿床地质特征及其成因

来源期刊：黄金2011年第1期

论文作者：郝通顺 王可勇 朴星海 万多 杨言辰 边红业

文章页码：25 - 28

关键词：青城子地区； 高家堡子银矿床； 小佟家堡子金矿床； 地质特征； 矿床成因

Key words：Qingchengzi area； Gaojiapuzi silver deposit； Xiaotongjiapuzi gold deposit； geological characteristic； genesis of ore deposit

摘    要：对辽宁青城子地区近年来发现的高家堡子银矿床及小佟家堡子金矿床地质特征及矿床成因进行了对比研究,结果表明两类矿床是在早期沉积-变质基础上,经历了后期热液叠加改造作用的结果,其中印支期岩浆热液活动导致了小佟家堡子等金矿床形成,而其后的大气降水活动是导致高家堡子银矿床富集成矿的主要机制。

Abstract: The comparative study on the geological characteristics and genesis of Xiaotongjiapuzi gold deposit and Gaojiapuzi silver deposit found in recent years in Qingchengzi area,Liaoning province were carried out.The results show that both of them are formed by the hydrothermal superimposition on the basement of sedimentation and metamorphism.The hydrothermal superimposition of the Indo-Chinese igneous activities led to the forming of the gold deposits in this area,while the superimposition of meteoric water gave rise to the silver deposits.