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沃溪金锑钨矿床稀土元素的研究表明：在成矿作用过程中，近矿脉围岩及矿层较远矿脉围岩发生了重稀土的迁出流失，稀土元素从赋矿围岩向含矿断裂带内定向迁移，断裂构造岩稀土元素的总含量与其构造破碎程度及所受的构造应力应变强度成正相关，成矿物质主要来自赋矿地层
The study of rare earth elements in the Woxi gold-antimony tungsten deposit shows that during the mineralization process, the heavy rare earths migrate out of the surrounding rocks near the ore bodies and the surrounding rocks in the distant ore layers, and the rare earth elements migrate from the ore-bearing rocks to the ore-bearing faults The total content of rare earth elements in tectonic rocks with directional migration and fracture is positively related to the tectonic crushing degree and the tectonic stress-strain intensity. The ore-forming materials mainly come from ore-bearing strata