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矿床地质  2010 

粤北红岭钨矿中辉钼矿Re-Os同位素年代学及其地质意义

Keywords: 地球化学,红岭钨矿,辉钼矿,Re-Os同位素,花岗岩,粤北

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Abstract:

粤北红岭钨矿为产在热水复式岩体之中的中型钨多金属矿床,矿化类型为石英脉型黑钨矿化和蚀变花岗岩型白钨矿化。对矿区含矿石英脉中8个辉钼矿样品进行Re-Os同位素测定,获得等时线年龄及模式年龄的加权平均值分别为(159.1±1.5)Ma和(158.8±0.88)Ma。等时线纵截距为-0.010±0.041,说明样品中不存在可测定的初始187Os。统计表明南岭地区中东段钨锡矿床的成矿年龄多集中在150~160Ma。粤北已有的几个钨矿成矿年龄与区域燕山期花岗岩大规模侵位时期一致,表明南岭地区花岗岩成岩成矿可能不存在明显的时差。

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