Based on the studies of the REE and trace elements of igneous rocks, and the stable isotope and inclusions Of the ore bodies, this paper discusses the genesis of the dePOsit.
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本文在对比分析矿区火成岩(围岩)及含矿段岩矿石稀土元素、微量元素的基础上,结合矿石稳定同位素及包裹体特征对矿床成因作了探讨。
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