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广西平南县大旺铅锌矿地质特征及矿床成因探讨

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广西平南县大旺铅锌矿位于钦杭成矿带西段,南华活动带的大瑶山隆起南部,处于区域性灵山-藤县断裂与凭祥-大黎断裂所夹持的沉积盆地中,该区地质构造复杂,成矿条件优越,通过对该区地质特征、矿化特征、找矿标志、矿床成因等的总结研究,认为大旺矿区属海底喷流沉积型为主叠加后期热液改造的铅锌矿床,可为区域上找同类型矿床提供参考.
Geological characteristics and genesis of Dawang lead-zinc deposit in Pingnan County,Guangxi
The Dawang lead-zinc deposit in Pingnan County,Guangxi is located in the western section of the Qinhang mineralization belt,in the southern part of the Dayaoshan uplift of the Nanhua active zone.It is situated in a sedimentary basin sandwiched between the regional Lingshan Tengxian fault and the Pingxiang Dali fault.The geological structure of the area is complex,and the mineralization conditions are superior.Through summarizing and studying the geological characteristics,mineralization characteristics,prospecting indicators,and genesis of the deposit in the area,It is believed that the Dawang mining area belongs to a lead-zinc deposit mainly composed of submarine jet sedimentation and later hydrothermal transformation,which can provide reference for finding similar deposits in the region.

Dawang lead-zinc mine in Pingnan County,GuangxiGeological characteristicsGenesis of mineral deposits

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广西壮族自治区三〇七核地质大队,广西 贵港 537100

广西平南县大旺铅锌矿 地质特征 矿床成因

2024

世界有色金属
有色金属技术经济研究院

世界有色金属

影响因子:0.138
ISSN:1002-5065
年,卷(期):2024.(1)
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