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REE characteristics in Guanpo- Wulichuan antimony belt in Lushi,Henan Province and its association with metallogenesis

Xiao Guangfu;Wu Luchuan;Zhongyuan Mining Co.,Ltd.,China National Gold Group Corporation;  
In order to study the ore-forming mechanism of Guanpo- Wulichuan antimony belt in Lushi,Henan Province,REE geochemical characteristics are analyzed. Light and heavy REE ratio in antimony ores and other type rocks in the belt is relatively high and displays an Eu negative anomaly. The allocation of REE generally takes the form of enrichment of light REE. Certain regularities exist in REE distribution in all kinds of rocks(ores) in the belt. Total amounts of REE content in marbles and antimony ores are higher while lower in ores in tectonic belt and its surrounding rocks,indicating that antimony and its ore-forming fluids mainly come from lower crust and upper mantle. When the fluids rose,they went through many stages of fractionation and metasomatic replacement,making REE displaced from the surrounding rocks and enriched in the deposit.
【CateGory Index】: P618.66;P595
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