矿物包体水中氢氧稳定同位素分析

    OXYGEN AND HYDROGEN STABLE ISOTOPIC ANALYSIS IN THE FLUID INCLUSION OF MINERALS

    • 摘要: 本文采用加温爆破法提取矿物的包体水。包体水中氘的分析采用金属铀法,氧—18的分析采用五氟化澳法。对金属铀法分析水的精密度和准确度进行了检查,δD值的平均偏差为±1.2‰,对北大自来水分析所得的δD值与镁粉法测定的δD值结果相符。不同矿物样品中包体水的重复测定表明,δD的偏差不超过2.5‰,δ~(18)O的偏差约为0.5‰。

       

      Abstract: The explosive method at elevated temperature is used for releasing inclusion water of mineral samples, and deuterium analyses of the water are performed using the metallic uranium method, while oxygen-18 analyses are made by reaction of the water with bromine pentafluoride. The precision and accuracy in the deuterium measurements are investigated. The mean deviation is±1.2‰. The result of this method is compatible with the data determined by the method of Mg powder reduction. Replicate analysis are made for the inclusion water in serveral samples and the D reported are precise to±2.5‰ and the deviation of 18O is±0.5‰.

       

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