| 浑南地区构造演化与金成矿关系讨论 |
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| 引用本文： | 赵永利.浑南地区构造演化与金成矿关系讨论[J].国土资源,1999(2). |
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| 作者姓名： | 赵永利 |
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| 作者单位： | 辽宁地质矿产勘查开发局第十地质大队 |
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| 摘 要： | 浑南位于华北地台，辽东台背斜铁岭－靖宇古隆起西部。区内浑河断裂及次级苏子河断裂的多期次活动控制了岩浆活动、火山喷发，以及矿产的分布。浑南地区金成矿分布主要集中在南口前及三块石花岗岩体周围，形成了南口前地区以金矿化为主，三块石（下营子—马尔墩）一带以金、银多金属矿化为主的成矿演化序列。
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| 关 键 词： | 构造演化 控矿 容矿构造 特征 金矿 |
ON THE RELATIONSHIP OF TECTONIC EVOLUTION OF THE AREA TO THE SOUTH OF HUNHE RIVER (HUNNAN AREA) IN LIAONING WITH GOLD METALLOGENESIS |
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| ZHAO Yong,li.ON THE RELATIONSHIP OF TECTONIC EVOLUTION OF THE AREA TO THE SOUTH OF HUNHE RIVER (HUNNAN AREA) IN LIAONING WITH GOLD METALLOGENESIS[J].Land & Resources,1999(2). |
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| Authors: | ZHAO Yong li |
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| Abstract: | Hunnan area,as one of the major metallogenic zones, locates in the west of Tieling Jingyu uplift of Liaodong anticline in the North China platform, in which multiphase activities of Hunhe fault and subsidiary Suzihe fault controlled magmatic activities,volcanic eruption and distribution of deposits.Gold deposits in Hunnan area mainly concentrated in Nankouqian (mainly taking place Au mineralization)and around the Sankuaishi granite body(mainly taking place Au Ag polymetallic mineralization). |
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| Keywords: | tectonic evolution ore controlling host structure characteristics gold deposit |
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