陕西省华阳川铀铌铅矿床碳酸岩岩石学及地球化学特征

Geoscience(2017)

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Abstract
陕西省华阳川铀铌铅矿床是小秦岭成矿带中成矿特征最为独特的矿床,碳酸岩脉的破碎带是重要的成矿空间.未矿化的碳酸岩中矿物以方解石为主,其他矿物很少;发育铀矿化的碳酸岩脉中矿物种类繁多,大部分为方解石,其次为角闪石、金云母、榍石、褐帘石、铌钛铀矿、重晶石、磷灰石、石英、磁铁矿、碱性长石等矿物.碳酸岩的LREE含量异常高,δ13CV-PDB和δ180V-SMOW值显示典型的火成碳酸岩特征.基于碳酸岩脉的Sr、Nd、Pb同位素比值(87 Sr/86 Sr-206 pb/204 Pb、207 pb/204 Pb-206 pb/204 Pb-143 Nd/1a Nd-87 Sr/86 St)的关系图,初步判断华阳川铀铌铅碳酸岩脉是源于EMI的碱性硅酸盐-碳酸盐熔体-溶液结晶分异的产物.
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Key words
carbonate vein,petrology,REE,isotopic geochemistry,Huayangchuan U-Nb-Pb deposit,Shaanxi Province
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