川西南马边地区萤石矿床成矿物质来源及其对区域找矿的启示

    Sources of ore-forming materials of fluorite deposit in the Mabian area, Southwest Sichuan, and implications for regional prospecting of fluorite

    • 摘要:
      研究目的 随着勘查工作的深入,川西南马边地区建立了磷-铅锌-萤石矿找矿新模型,相关铅锌矿中伴生的萤石矿逐渐被报道,但区内萤石矿在成矿物质来源的系统地球化学研究和成矿模式上仍存在显著空白。探讨川西南马边地区萤石矿的成矿物质来源及矿床成因,为指导区域找矿提供理论依据。
      研究方法 在矿床地质特征研究的基础上,对马边地区萤石矿含矿岩系及下伏磷矿层进行了系统的地球化学研究。
      研究结果 萤石呈脉状、不规则团块状不均匀分布于铅锌矿体中,赋存于寒武系纽芬兰统筇竹寺组断层或张性裂隙中。综合微量元素、稀土元素和同位素地球化学特征等,认为萤石矿的成矿流体主要为地下热卤水和少量天然热水,成矿物质中的Ca主要来源为上震旦统灯影组和寒武系纽芬兰统麦地坪组的碳酸盐岩,成矿物质中的F主要来源于寒武系纽芬兰统麦地坪组含氟磷块岩,矿床类型属于中低温热液充填型矿床。
      结论 四川极度缺乏萤石矿资源,属无萤石成矿区带,但研究认为区域峨边-金阳大断裂的次级断裂构造为重要成矿构造,据此提出在四川马边—雷波—金阳—布拖一带部署新一轮找矿突破战略行动,该区域有望实现中国西南地区萤石矿找矿突破。

       

      Abstract:
      This paper is the result of geochemistry of ore deposits and metallogenic models.
      Objective With the advancement of exploration work, a new model for phosphate−lead−zinc−fluorite mineral exploration has been established in the Mabian region, southwestern Sichuan Province. Reports of fluorite minerals occurring in association with lead−zinc deposits have begun to emerge. However, there are still significant gaps in the systematic geochemical studies of ore−forming material sources and metallogenic models of fluorite deposits in this area. The purpose of this paper is to discuss the source of mineralization and genesis of the fluorite deposit in Mabian area, Southwest Sichuan, and provide theoretical basis for regional prospecting.
      Methods Based on the geological characteristics of the deposit, this paper conducts a systematic study on geochemistry of the fluorite−bearing rock series and the underlying phosphate layers in the Mabian area.
      Results Fluorite occurs in vein−like and irregular lump−like patterns unevenly distributed within the lead−zinc deposits, and is produced in the faults or tensile fractures of Qiongzhusi Formation of Cambrian Terreneuvian series. Based on the trace elements, rare earth elements and isotope geochemical characteristics, it is believed that the mineralizing fluids of the fluorite deposit are mainly underground brine and a small amount of natural hot water, and that the main sources of Ca for the mineralization are the carbonate rocks in Dengying Formation of Upper Sinian series and the Maidiping Formation of Cambrian Terreneuvian series, while the main source of F for the mineralization is the fluorite phosphate rock of the Maidiping Formation of the Cambrian Terreneuvian series. The type of deposit is a medium−low temperature hydrothermal filling type deposit.
      Conclusions The fluorite resources are extremely scarce in Sichuam, placing it within a non−fluorite metallogenic belt. This research believes that the secondary fault structure of the Ebian−Jinyang major fault is an important mineralizing structure, and that deploying a new round of fluorite mineral exploration project in the area of Mabian−Leibo−Jinyang−Butuo in Sichuan Province has better prospects for mineral exploration, which is expected to achieve a breakthrough in fluorite prospecting in Southwest China.

       

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