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试论随州吴山铜钼多金属矿地质特征及找矿方向

On the geological characteristics and prospecting direction of the Wushan copper molybdenum polymetallic deposit in Suizhou
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摘要 吴山铜钼多金属矿主要分布在桐柏-大别山钼多金属成矿带西南部的区段上,区内有着较为复杂的地层产出,并有着频繁而又强烈的构造岩浆活动,成矿地质条件优越。下文中主要对该矿成矿地质特征进行详细分析和阐述,在此基础上,探究分析该矿矿床成因,并对找矿标志进行总结指出今后的找矿方向,希望能对区内地质找矿工作提供一些指示作用。 The Wushan copper molybdenum polymetallic deposit is mainly distributed in the southwestern section of the Tongbai Dabie Mountain molybdenum polymetallic mineralization belt.There are complex stratigraphic outputs and frequent and strong tectonic magmatic activities in the area,with superior geological conditions for mineralization.The following text mainly provides a detailed analysis and exposition of the geological characteristics of the ore deposit.Based on this,the genesis of the ore deposit is explored and analyzed,and the prospecting indicators are summarized to point out the future prospecting direction.It is hoped that this can provide some guidance for the geological prospecting work in the area.
作者 李冰洋 袁灵攀 林紫坤 LI Bing-yang;YUAN Ling-pan;LIN Zi-kun(Eighth Geological Brigade of Hubei,Xiangyang 441001,China)
出处 《世界有色金属》 2024年第8期129-131,共3页 World Nonferrous Metals
关键词 吴山铜钼多金属矿 地质特征 找矿方向 随州 Wushan copper molybdenum polymetallic ore Geological characteristics Exploration direction Suizhou
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