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对湖南沃溪金锑钨矿床稀土元素特征的研究结果表明 :在成矿过程中 ,稀土元素发生了从近矿围岩向含矿断裂带或成矿热液的迁移 ;成矿物质主要来自赋矿地层围岩 ,且具多源性 ;矿化程度不同的层脉石英矿石中的稀土总含量具有明显的差异。同时指出了将热液金矿床中石英脉内稀土总含量作为找矿标志的可能性。
The results of REE characteristics of the Woxi gold-antimony-tungsten deposit in Hunan Province show that during the mineralization process, the migration of rare earth elements from the ore-bearing rocks to the ore-bearing fault zones or ore-forming hydrothermal fluids occurs. The metallogenic materials mainly come from the Fu There are multi-source rocks in the ore strata. There is a clear difference in the total content of rare earths in the strata-quartz ore with different degrees of mineralization. At the same time, the possibility of using the total rare earth content in the quartz vein in the hydrothermal gold deposit as a prospecting indicator is also pointed out.