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首页> 外文期刊>Doklady Earth Sciences >U—Pb Age and Sr-Chemostratigraphy of Limestone from the Sorna Formation, Azyr—Tal Range, Kuznetsk Alatau
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U—Pb Age and Sr-Chemostratigraphy of Limestone from the Sorna Formation, Azyr—Tal Range, Kuznetsk Alatau

机译:库兹涅茨克阿拉托Azyr-Tal山脉索尔纳组石灰岩的U-Pb年龄和Sr-化学地层学

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The U-Pb(Pb-Pb) age was determined for limestone from member III of the Sorna Formation outcropped on the Azyr-Tal Range, Kuznetsk Alatau. The weighted average value from three calculated values is 523 ± 5 Ma (MSWD = 0.02,2a). This age coincides with the Early Cambrian age interval determined with Sr iso-topic chemostratigraphy (~(87)Sr/~(86)Sr ratio is 0.70850-0.70852). The low value of μ_2 = ~(238)U/~(204)Pb for limestone is due to the evolution of diagenetic fluid containing lead from the mantle reservoir into the Sorna sediments.
机译:确定了在库兹涅茨克阿拉托的Azyr-Tal山脉露头的Sorna组成员III的石灰岩的U-Pb(Pb-Pb)年龄。来自三个计算值的加权平均值为523±5 Ma(MSWD = 0.02,2a)。该年龄与用Sr同位素化学地层学确定的早寒武纪年龄间隔一致(〜(87)Sr /〜(86)Sr比为0.70850-0.70852)。石灰岩的μ_2=〜(238)U /〜(204)Pb的较低值是由于含铅的成岩流体从地幔储层向索尔纳沉积物中的演化。

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    《Doklady Earth Sciences 》 |2011年第1期| p.331-334| 共4页
  • 作者单位

    Institute of Precambrian Geology and Geochronology,Russian Academy of Sciences, nab. Makarova 2,St. Petersburg, 199034 Russia;

    Institute of Precambrian Geology and Geochronology,Russian Academy of Sciences, nab. Makarova 2,St. Petersburg, 199034 Russia;

    Institute of Precambrian Geology and Geochronology,Russian Academy of Sciences, nab. Makarova 2,St. Petersburg, 199034 Russia;

    Sobolev Institute of Geology and Mineralogy, SiberianBranch, Russian Academy of Sciences,pr. Akademika Koptyuga 3, Novosibirsk, 630090 Russia;

    Institute of Precambrian Geology and Geochronology,Russian Academy of Sciences, nab. Makarova 2,St. Petersburg, 199034 Russia;

    Institute of Precambrian Geology and Geochronology,Russian Academy of Sciences, nab. Makarova 2,St. Petersburg, 199034 Russia;

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