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

    THERMODYNAMIC PROPERTIES OF ESR SIGNALS OF DEEP-SEA CARBONATE

    • 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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