刁少波, 贺行良, 何乐龙, 张道来, 张剑, 李建平. 深海碳酸盐岩ESR测年信号的热力学特征[J]. 海洋地质前沿, 2018, 34(8): 1-6. DOI: 10.16028/j.1009-2722.2018.08001
    引用本文: 刁少波, 贺行良, 何乐龙, 张道来, 张剑, 李建平. 深海碳酸盐岩ESR测年信号的热力学特征[J]. 海洋地质前沿, 2018, 34(8): 1-6. DOI: 10.16028/j.1009-2722.2018.08001
    DIAO Shaobo, HE Xingliang, HE Lelong, ZHANG Daolai, ZHANG Jian, LI Jianping. THERMODYNAMIC PROPERTIES OF ESR SIGNALS OF DEEP-SEA CARBONATE[J]. Marine Geology Frontiers, 2018, 34(8): 1-6. DOI: 10.16028/j.1009-2722.2018.08001
    Citation: DIAO Shaobo, HE Xingliang, HE Lelong, ZHANG Daolai, ZHANG Jian, LI Jianping. THERMODYNAMIC PROPERTIES OF ESR SIGNALS OF DEEP-SEA CARBONATE[J]. Marine Geology Frontiers, 2018, 34(8): 1-6. DOI: 10.16028/j.1009-2722.2018.08001

    深海碳酸盐岩ESR测年信号的热力学特征

    THERMODYNAMIC PROPERTIES OF ESR SIGNALS OF DEEP-SEA CARBONATE

    • 摘要: ESR测年方法的年代范围可以从数百年到几百万年,但在较老的深海碳酸盐岩测年研究中,ESR测年信号的平均寿命较短,其年龄极限受到质疑。利用较老的深海碳酸盐岩进行了ESR测年信号的热力学特征研究,同时估算了深海碳酸盐岩的平均寿命。研究结果表明:单一级热动力学模式不适于深海碳酸盐岩样品的平均寿命估算,而双一级动力学模式是一种较好的估算方法。经估算,深海碳酸盐岩试样的平均寿命为5.14 Ma,年龄为320±50 ka,与铀系不平衡法测得的365±49 ka具有较好的一致性。

       

      Abstract: The ESR dating method could date the samples within a time span from hundreds of years to millions of years. However, the average lifetime of ESR signals from deep-sea carbonate rocks are relatively shorter. In this regard, the age limit of the deep-sea carbonate rocks dating need to be further studied. In this paper, we studied the thermodynamic characteristics of ESR dating signals acquired from old deep-sea carbonate rocks and the average lifetime of those deep-sea carbonate rocks is estimated. The results of the thermodynamic properties of deep-sea carbonate suggests that the single first-order kinetic equation might not be suitable to calculate the average lifetime, and the double first-order kinetic equation is more effective. The average lifetime of the deep-sea samples we calculated is about 5.14×106 years by using the double first-order kinetic equation. Thus the estimated age is 320±50 ka, which is in good agreement with the unbalanced U system dating result of 365±49 ka.

       

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