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《Geological Review》 1991-02
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ESR AND URANIUM SERIES AGES OF HOLOCENE CORAL REEFS IN THE SOUTH CHINA SEA

Ye Yuguang, He Jie, Diao Shaobo and Liu Xinbo (Institute of Marine Geology, Ministry of Geology and Mineral Resources, Qingdao) Gao Juncheng and Du Yajing (National Institute of Metrology, Beijing)  
The ages of 14 samples of coral reefs from several shallow drilling holes in the South China Sea were determined by both ESR and uranium series (~(230)Th/~(234)U) methods, and the experimental results show ideal agreement between ESR and uranium series data. These coral reefs formed in the early part of the Holocene.It was found that the effects of magnetic saturation of the samples were different from each other in this research. In the determination of the natural total dose of the coral reef by use of the additive dose method satisfactory resultswere obtained using the exponential fitting.Different α radiant efficiencies——k values——should be selected for different samples because of the different effects of the magnetic saturation of various samples. There is an obvious positive correlation between the k value and the ratio of the natural ESR signal intensity (I_0) to the ESR signal intensity of magnetic saturation (I_(max)) of the samples. Based on some ESR ages of samples in chemical closure systems and the ratios of I_0/I_(max), a linear equation for determining the k value can be obtained; k=4.386×I_0/I_(max)+0.095. Employing the formula the k value of the samples can be given readily. The use of the formula is advantageous to improve the precision of ESR dating of marine carbonates.
【Fund】: 本项研究为地质行业科学技术发展基金(编号88121)
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