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作 者:徐明璞 解天赐 刘天鹏 王鲁艳 孙雪飞 Xu Mingpu;Xie Tianci;Liu Tianpeng;Wang Luyan;Sun Xuefei(No.6 Geological Team of Shandong Provincial Bureau of Geology and Mineral Resources(No.6 Institute of Geology and Mineral Resources Exploration of Shandong Province),Weihai Shandong 264200,China;Shandong Province Deep Gold Mine Exploration Big Data Application Development Engineering Laboratory,Weihai Shandong 264200,China)
机构地区:[1]山东省地质矿产勘查开发局第六地质大队(山东省第六地质矿产勘查院),山东威海264200 [2]山东省深部金矿探测大数据应用开发工程实验室,山东威海264200
出 处:《山西冶金》2024年第5期57-59,91,共4页Shanxi Metallurgy
基 金:山东省地矿局2022年度科技攻关项目:招平断裂带中段深部金矿资源潜力调查项目(KC202210);胶西北断裂系统及其成矿关系项目(KY202208)。
摘 要:招(远)—平(度)断裂带作为胶东三大主要金成矿带之一,历来备受学者关注。但是,关注焦点大都汇聚于招(远)—平(度)断裂带,而对其下盘的次级蚀变带却不够重视。基于此,依据玲南矿区地质成果报告,结合玲南矿区地质背景,分析研究断裂带下盘的1号、2号蚀变带赋存矿体及围岩蚀变等特征,总结金矿物的形态及赋存状态,明确了找矿标志和成因等因素,阐明了1号、2号蚀变带找矿意义和赋矿潜力,对深部找矿具有一定的指导意义。The Zhaoyuan-Pingdu fault zone,as one of the three major gold mineralization zones in Jiaodong,has always been of great concern to scholars.However,most of the focus is on the Zhaoyuan-Pingdu fault zone,while the secondary alteration zone in its footwall is not given enough attention.Based on this,based on the geological aievemencht report of Lingnan mining area and combined with the geological background of Lingnan mining area,the characteristics of the occurrence of ore bodies and surrounding rock alteration in the No.1 and No.2 alteration zones under the fault zone are analyzed and studied.The morphology and occurrence status of gold minerals are summarized,and factors such as prospecting indicators and genesis are clarified.The significance and potential of prospecting in the No.1 and No.2 alteration zones are elucidated,which has certain guiding significance for deep prospecting.
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