贵州桐梓县石门坎锂矿区地质特征及找矿潜力

    Geological characteristics and prospecting potential of Shimenkan lithium mining area in Tongzi County of Guizhou Province

    • 摘要: 石门坎锂矿区位于毕节弧形褶皱带与凤岗SN向隔槽式褶皱变形区的结合部位,锂矿找矿潜力较好。在桐梓县石门坎及周边地区实施1∶ 1万矿产地质填图,开展浅部剥土、探槽工程和深部钻探工程。通过收集来自矿产调查地质点、剥土工程、探槽工程及钻孔的40个厚度数据,利用MapGIS空间DTM自动分析功能,生成含锂岩系等厚线。结果显示: 初步圈定1个锂矿体,矿体总体呈NNE—SSW向展布,矿体走向平均为28°,Li2O加权平均品位为0.31%。综合分析表明: 区域上大竹园组厚度呈北厚南薄的特点,南部黔北平原隆起导致含锂岩系的缺失,木瓜镇以北的石门坎地区和坡渡镇以西的藻渡地区成矿条件较好,含锂岩系厚度大、品位高,具有较好的锂矿找矿潜力。研究成果对石门坎及周边地区锂矿找矿勘查具有地质指示意义。

       

      Abstract: Shimenkan lithium mining area is located at the junction of Bijie arc-shaped fold belt and Fenggang north-south trough type fold deformation zone, with good potential for lithium ore exploration. The 1∶ 10 000 mineral geological mapping was implemented in Shimenkan and its the surrounding areas of Tongzi County, and shallow soil stripping, trench exploration, and deep drilling projects were also carried out. By collecting 40 thickness data geological points, soil stripping, trench exploration, and drilling prejects, the authors utilized the automatic analysis function of MapGIS spatial DTM to generate of lithium bearing rock series ispach lines. The results show that one lithium ore body has been preliminarily delineated. The ore body is generally distributed in NNE-SSW direction, with a strike of 28° and a weighted Li2O grade of 0.31%. Comprehensive analysis shows that the thickness of Dazhuyuan Formation in the region is characterized by being thicker in the north and thinner in the south. The uplift of Qianbei Plain in the south leads to the absence of lithium bearing rock formations. Two areas have better mineralization conditions, including Shimenkan area in north of Mugua Toun, and Zaodu area in west of Podu Town, with thick and high-grade lithium bearing rock formations and good potential for lithium mineral exploration. The research results could provide geological significance for lithium ore exploration in Shimenkan and its surrounding areas.

       

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