芦子园铜铅锌多金属矿床地质特征及成因分析  

Geological characteristics and genesis analysis of the Luziyuan copper lead zinc polymetallic deposit

作　　者：吴邦天 WU Bang-tian(Yunnan Nonferrous Geological Bureau 306 Team,Kunming 650000,China)

机构地区：[1]云南省有色地质局三0六队,云南昆明650000

出　　处：《世界有色金属》2025年第1期70-72,共3页World Nonferrous Metals

摘　　要：芦子园铜铅锌多金属矿区位于冈底斯-喜马拉雅造山系保山地块的永德陆表海。区域地质构造复杂,构造主要为镇康复背斜。地壳厚度大,地质构造演化历史复杂,成矿条件十分有利。对矿区地质特征和矿床成因进行分析,并对矿区范围内矿体形态、资源量、矿石质量成分及成因进行粗浅的分析,提出下一步找矿方向和思路。The Luziyuan copper lead zinc polymetallic mining area is located in the Yongde Land Surface Sea of the Baoshan Block of the Gangdise Himalayan orogenic system.The regional geological structure is complex,with the main structure being the Zhenfukang anticline.The thickness of the crust is large,the geological structure evolution history is complex,and the mineralization conditions are very favorable.Analyze the geological characteristics and genesis of the mining area,and conduct a preliminary analysis of the morphology,resource quantity,ore quality composition,and genesis of the ore body within the mining area.Propose the next direction and ideas for mineral exploration.

关 键 词：铜铅锌矿 地质特征 成矿规律 芦子园 

分 类 号：P618.2[天文地球—矿床学]