李存有, 施立达. 包裹体爆裂法测试中石英α-β峰的产生原因及找矿意义[J]. 地质与资源, 1999, 8(1): 35-37. DOI: 10.13686/j.cnki.dzyzy.1999.01.007
    引用本文: 李存有, 施立达. 包裹体爆裂法测试中石英α-β峰的产生原因及找矿意义[J]. 地质与资源, 1999, 8(1): 35-37. DOI: 10.13686/j.cnki.dzyzy.1999.01.007
    Li Cunyou, Shi Lida. THE REASON AND EXPLORING SIGNIFICANCE OF α β PEAK OF QUARTZ IN DECREPITATION TEST[J]. Geology and Resources, 1999, 8(1): 35-37. DOI: 10.13686/j.cnki.dzyzy.1999.01.007
    Citation: Li Cunyou, Shi Lida. THE REASON AND EXPLORING SIGNIFICANCE OF α β PEAK OF QUARTZ IN DECREPITATION TEST[J]. Geology and Resources, 1999, 8(1): 35-37. DOI: 10.13686/j.cnki.dzyzy.1999.01.007

    包裹体爆裂法测试中石英α-β峰的产生原因及找矿意义

    THE REASON AND EXPLORING SIGNIFICANCE OF α β PEAK OF QUARTZ IN DECREPITATION TEST

    • 摘要: 石英在爆裂法测试中常出现α-β峰,此峰是由爆裂温度大于573℃的高温流体包裹体,在α石英相变成β石英时,包裹体发生泄漏(非爆裂)形成的.在金矿地质找矿中,用α-β峰可判断矿脉的剥蚀程度,推测矿床成因

       

      Abstract: In decrepitation test for quartz,α-β peaks frequently appear when the samples are heated to the temperature of 573℃.Study shows that the α-β peak is produced by the leaking(without decrepitating) of high temperature inclusions whose decrepitating temperature is higher than 573℃,the critical point when α quartz converts into β quartz This form of peak may be used to infer the denuded degree of lodes and decide the origin of deposits in gold ore exploring

       

    /

    返回文章
    返回