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陕县宽坪银多金属矿区地质特征与成矿规律
引用本文:杨林楠,陈静,冯昂,李钢.陕县宽坪银多金属矿区地质特征与成矿规律[J].矿产与地质,2016(3):344-347.
作者姓名:杨林楠  陈静  冯昂  李钢
作者单位:河南省有色金属地质矿产局第一地质大队,河南 郑州,450016
摘    要:陕县宽坪银多金属矿位于崤山矿集区内,已探明银铅锌储量达中等以上规模。通过研究矿区地质特征,认为矿体主要受构造蚀变带控制,在含矿热液的多期、多阶段交代和充填作用下,在构造有利部位富集成矿。

关 键 词:银多金属矿  构造蚀变带  含矿热液  成矿规律

Geological characteristics and metallogenic regularity of Kuanping Ag polymetallic mining area in Shanxian
Abstract:Kuanping Ag polymetallic deposit is located in Xiaoshan ore-concentrated area with verified silver-lead-zinc reserves which are up to medium scale and above.Through studies on the geological characteristics of the mining area,the author believed that the orebodies were controlled by tectonic alternation zone.Under the influence of filling-metasomatism of ore-bearing hydrothermal fluid in multiple stages and periods,ores are enriched and mineralized at favorable parts of the structure.
Keywords:Ag polymetallic deposit  tectonic alternation zone  ore-bearing hydrothermal fluid  metallogenic regularity
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