贵州遵义团溪地区铝土矿矿地质特征与找矿潜力探讨被引量：2

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摘要研究区从中奥陶世—中石炭世期间,地壳处于抬升状态,形成大面积的古风化壳,接受陆相沉积,为区内铝土岩含矿地层形成提供了充足的物源条件而形成了大面积含矿地层,在这些含矿地层中找铝土矿的潜力巨大;区内地质构造发育,岩石破碎,可作为良好的导水系统,对含矿岩系铝土岩起到良好的淋漓作用,使铝土岩受淋漓作用而再次富集成矿.在研究区F1断层到F2断层之间以及F1断层南东区域大面积含矿地层具有较大的找矿潜力;区内碎屑状、半土状铝土矿品位较好,而区内含矿岩系中广泛出露碎屑状、半土状铝土岩,推测区具有较大的找矿潜力.

作者鲍淼林权富张继银

机构地区贵州省地矿局一一二地质大队

出处《西部探矿工程》 CAS 2020年第8期111-114,共4页 West-China Exploration Engineering

关键词铝土矿地质特征找矿潜力团溪遵义贵州

分类号 P619 [天文地球—矿床学]

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