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A practical method for determination of molybdenite Re-Os age by inductively coupled plasma-mass spectrometry combined with Carius tube-HNO3 digestion

机译:电感耦合等离子体质谱-Carius管-HNO3消解法测定辉钼矿Re-Os年龄的实用方法

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摘要

A simplified method for the determination of molybdenite Re-Os ages using inductively coupled plasma-mass spectrometry (ICP-MS) is presented. By the means of Carius tube method, molybdenite and pyrite were digested using concentrated HNO3, and were then changed into MoO3 and Fe(NO3)3 precipitates, respectively. Rhenium was determined directly by ICP-MS after removal of Os by heating for the molybdenite supernatant or by cation-exchange purification for the pyrite supernatant. Osmium distilled as OsO4 from the supernatant was trapped using pure water and could be directly analyzed by ICP-MS. This method was validated using two molybdenite reference materials, GBW 04435 and GBW 04436, and their Re-Os ages obtained are 220.3 ± 1.1 Ma (1.0%, 2s), and 140.5 ± 0.9 Ma (1.2%, 2s), respectively, consistent with literature values. The proposed Re-Os dating method was applied to molybdenite and pyrite sampled from a porphyry Mo-deposit. The results show that this deposit is the oldest Mo-deposit so far found in China.
机译:提出了一种使用电感耦合等离子体质谱法(ICP-MS)测定辉钼矿Re-Os年龄的简化方法。通过Carius管法,用浓HNO3消化辉钼矿和黄铁矿,然后分别转化为MoO3和Fe(NO3)3沉淀。 heating在去除Os后,通过加热用于辉钼矿上清液或通过阳离子交换纯化用于黄铁矿上清液,直接通过ICP-MS测定hen。用纯水捕获从上清液中蒸馏出的O,以OsO4的形式收集,可以通过ICP-MS直接分析。使用两种辉钼矿参考材料GBW 04435和GBW 04436对该方法进行了验证,其获得的Re-Os年龄分别为220.3±1.1 Ma(1.0%,2s)和140.5±0.9 Ma(1.2%,2s),一致具有文学价值。提出的Re-Os定年方法适用于斑岩型钼矿床中的辉钼矿和黄铁矿。结果表明,该矿床是迄今为止中国发现的最古老的钼矿床。

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