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作 者:张大伟 ZHANG Da-wei(Liaoning Nonferrous Geology 105 Team Co.,Ltd.,Huludao 125000,China)
机构地区:[1]辽宁省有色地质一〇五队有限责任公司,辽宁葫芦岛125000
出 处:《有色矿冶》2023年第1期1-4,共4页Non-Ferrous Mining and Metallurgy
摘 要:小孤山金矿和西双山铜金多金属矿均位于青龙—锦西火山热液成矿带上,两个矿区直线距离仅3 km。在充分收集两个矿区地质资料的基础上,结合近期找矿工作成果,对两个矿区的地质、物探、化探特征进行对比分析,建立双山成矿模型,为在该区域的找矿工作提供思路。The Xiaogushan gold deposit and Xishuangshan cop-gold polymetallic deposit are located in the QinglongJinxi volcanic hydrothermal metallogenic belt,and the straight-line distance between the two mining areas is only 3km.On the basis of fully collecting the basic geological data of the two mining areas and combining with the recent prospecting results,the geological,geophysical and geochemical characteristics of the two mining areas are compared and analyzed,and the Shuangshan metallogenic model is established,which provides ideas for the prospecting work in this area.
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