于莱州湾南岸ZK32-1钻孔第三陆相层上下边界处选取自生钙质结核,采用样品全溶铀系等时线法(TSD法)测定钙质结核的年龄。测试结果表明,所有等时线上的数据都有很好的线性关系,表明所获得的年龄数据是合理的。通过对样品代表性的讨论,说明所选取的钙质结核的年龄确可代表其所在地层的年龄,从而得出莱州湾南岸第三陆相层的沉积起止时间为72.16kaB.P.±7.41kaB.P到45.34kaB.P.±5.35kaB.P.的结论。本研究首次获得莱州湾南岸地层的铀系TSD年龄,为全面认识该地区晚更新世地层年代学提供了一个新视角。
In order to know the age of the third continental facies of the south coast of Laizhou Bay, authigenic calcrete nodules existed in the core ZK32-1 were sampled. The nodules existed in the layes and determined by the total-sample-dissolution isochron (TSD) techniques can be represented. The ages are 45.34 ka B.P.±5.35ka B.P. and 72.16 ka B.P.±7.41 ka B.E for the top and base layers of the continental facies respectively. They're the first TSD data and consistent with previous research.