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    四川省瓦岗地区水系沉积物地球化学特征及找矿方向

    Geochemical characteristics of stream sediments and prospecting directions in Wagang area of Sichuan Province

    • 摘要: 四川省瓦岗地区位于川西南—滇东北地区的结合部位,所处的乌蒙山区是我国著名的扬子式铅锌矿带的核心区,也是全国重要的磷成矿带,具有较好的找矿潜力。文章通过开展瓦岗地区1∶5万水系沉积物地球化学测量工作,结合研究区地质背景,对区内与优势矿种相关的11种元素(Pb、Zn、Ag、Cd、P、F、Mn、Au、As、Sb、Hg)的地球化学特征进行研究,通过聚类分析和因子分析确定元素组合异常,进而圈定成矿综合异常。结果表明:区内磷、铅、锌元素异常高值点较多,离散程度高,异常高值与赋矿地层套合较好,具有较大的成矿潜力;主攻矿种为沉积型磷矿,兼顾铅锌矿和锑矿,其中磷矿主要产于震旦纪—寒武纪渔户村组中谊村段,铅锌矿主要赋存于渔户村组上部;区内共圈定6个综合异常,可为下一步找矿工作提供依据。

       

      Abstract: The Wagang area is located on the border of southwestern Sichuan and northeastern Yunnan, belonging to Wumeng Mountain, which is the famous core area of the Yangtze platform, as well as an important phosphorus metallogenic belt in China with good prospecting potential. Based on the 1:50000 stream sediment survey in the Wagang area, this paper described geochemical characteristics of 11 elements such as Pb, Zn, Ag, Cd, P, et al. Cluster analysis and factor analysis were utilized to determine the combined anomalies and the comprehensive anomalies. The results show that: there are many highly dispersive abnormal high value points of phosphorus, lead and zinc elements in the Wagang area. The abnormal high values are well matched with the ore bearing strata, and have great mineralization potential. The main type of minerals is sedimentary phosphorus ore, coupling with lead-zinc and antimony ores. Phosphorite is mainly occurred in the middle Yicun section of the Aurignacian-Cambrian Yuhucun Formation, while lead-zinc ores are developed in the upper part of the Yuhucun Formation. Combined with elements assemblages, abnormal characteristics and the ore-forming geological settings, the authors delineated 6 geochemical anomalies, which can provide important evidences for further prospecting.

       

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