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黄陵断穹某离子吸附型稀土矿点成矿地质特征

Resources Environment & Engineering(2021)

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Abstract
首次在黄陵断穹北部发现一处离子吸附型稀土矿点.通过总结该矿点地质特征,浅析其成因.研究表明,该矿点的成矿母岩为中太古代东冲河片麻杂岩,矿(化)体呈似层状赋存于东冲河片麻杂岩风化壳的全风化层中;具有较高稀土元素丰度的东冲河片麻杂岩、湿热气候、中低山较平缓地形等因素耦合造就成矿.该项研究可为区域离子吸附型稀土矿找矿勘查工作提供参考.
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