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    辽宁清原县大荒沟地区铁矿地质特征及找矿远景分析

    Geological characteristics and prospecting prospects of iron ore in the Dahuanggou area, Qingyuan County, Liaoning Province

    • 摘要: 清原县大荒沟地区铁矿赋存于新太古界清原岩群红透山岩组中,铁矿与围岩界线清晰。该区共圈定13条铁矿体,多呈层状、似层状、透镜状,矿床mFe平均品位21.61 %,TFe平均品位28.76 %。矿床成因类型为沉积变质型铁矿床,属鞍山式铁矿。本文通过对大荒沟地区铁矿地质特征进行全面总结和研究,初步建立找矿预测地质模型,对进一步深、边部找矿工作具有指导意义。

       

      Abstract: The iron ore in Dahuanggou area of Qingyuan county occurs in the Hongtoushan Formation , which belongs to Neoarchean Qingyuan Group. The boundaries between iron ore and surrounding rock are clear. A total of thirteen iron ore bodies have been delineated in this area, mostly occurring as layered, stratiform-like, and lenticular forms. The average grade of mFe and TFe is 21.61% and 28.76%, respectively. The genetic type of the deposit is classified as sedimentary-metamorphic iron deposit, belonging to the Anshan iron deposit. Through a comprehensive synthesis and study of the geological characteristics of the iron ore in the Dahuanggou area, and a preliminary prospecting prediction model is established, which offers guiding significance for further deep and peripheral prospecting work.

       

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