对贵州织金三甲地区寒武系底部戈仲伍组含磷岩系稀土元素、微量元素和一些常量元素等在剖面上的变化规律进行系统的研究, 并结合剖面上小壳动物化石富集特点, 认为寒武系底部戈仲伍组中有两个磷和稀土成矿期, 稀土含量与磷含量成显著的正相关关系, 而与小壳动物化石丰度没有显著相关性.
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