| 辽宁省吴家堡钼矿地质特征及找矿方向浅析 |
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| 引用本文： | 方磊,王永春,刘宪春,高飞.辽宁省吴家堡钼矿地质特征及找矿方向浅析[J].地质调查与研究,2011,34(2):119-125. |
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| 作者姓名： | 方磊 王永春 刘宪春 高飞 |
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| 作者单位： | 1. 辽宁工程技术大学,资源与环境工程学院,阜新123000
2. 辽宁省核工业地质局241大队,丹东,118100 |
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| 基金项目： | 中央地质勘查基金项目:辽宁省本溪县悬岭后铅锌金多金属矿普查(2007211005) |
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| 摘 要： | 吴家堡钼矿位于辽东裂谷北部本溪-凤城多金属成矿带的中部,主要产于古元古代碎斑状花岗岩构造裂隙中,钼成矿与中侏罗世白水寺花岗岩体侵入有关,与矿化有关的围岩蚀变主要为硅化、钾长石化、黄铁矿化及绢云母化,矿石矿物以辉钼矿为主。矿化类型主要为细脉浸染状,矿床具有斑岩型矿床的特征,找矿有利部位为中侏罗世花岗岩体与古元古代花岗岩体及辽河群地层接触外带,其矿化规模及找矿前景较好。
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| 关 键 词： | 吴家堡 钼矿 地质特征 找矿方向 辽宁省 |
Geological Characteristics and Prospecting Direction of the Wujiapu Molybdenum Deposit in Liaoning Province |
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| FANG Lei,WANG Yong-chun,LIU Xian-chun,Gao Fei.Geological Characteristics and Prospecting Direction of the Wujiapu Molybdenum Deposit in Liaoning Province[J].Geological Survey and Research,2011,34(2):119-125. |
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| Authors: | FANG Lei WANG Yong-chun LIU Xian-chun Gao Fei |
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| Institution: | FANG Lei1,WANG Yong-chun1,LIU Xian-chun2,Gao Fei(1.College of Resource and Environment Engineering,Liaoning Technical University,Fuxin 123000,China,2.The 241st Team of Liaoning Nuclear Geological Buteau,Dandong 118100,China) |
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| Abstract: | The Wujiapu molybdenum deposit is located in the center of the Benxi-Fengcheng molymetallic ore-forming belt in the northern part of the Liaodong rift.It is mainly occurs in the Paleoproterozoic porphyritic granite structural fissures.The molybdenum mineralization is related to the Late Jurassic Baishuisi granite invasion.The wallrock alteration with the mineralization is silicification,potassic,pyritization and sericitize.The ore minerals are chiefly molbdenites.The mineralization principally is the veinle... |
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| Keywords: | Wujiapu molybdenum deposit geological characteristic prospecting direction Liaoning Province |
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