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作 者:韩非[1,2] 尹功明[1] 刘春茹[1] 高璐[1]
机构地区:[1]中国地震局地质研究所,地震动力学国家重点实验室,北京100029 [2]法国国家自然历史博物馆史前部,1,rue Rene Panhard 75013,Paris,France
出 处:《核技术》2011年第9期651-657,共7页Nuclear Techniques
基 金:中央级公益性科研院所基本科研业务费(DF-IGCEA-0608-2-17);国家自然科学基金(40902051)资助
摘 要:介绍了电子自旋共振(ESR)法与铀系测年法联合对牙齿化石测年的基本原理,通过引入参数p反映牙齿化石中各组织的铀吸收过程;阐述了ESR-U系联合测年法的测年时限、测年精度及影响因素。对于我国中早更新世考古遗址的化石测年具有潜在优势,是目前唯一可行的对老地点化石样品进行直接测年的方法。In this paper, we give a review on combined ESR/U-series methods for dating tooth fossil from Middle-Early Pleistocene sites. This approach allows estimating the history of uranium uptake in each dental tissue by using a one-parameter (p-value) diffusion equation, being more accurate than the conventional methods where the mode of uranium uptake is predetermined. Conventional ESR dating postulates two models: an early uptake (EU) model which assumes that uranium was incorporated shortly after the sample burial, and a linear uptake (LU) model where uranium is supposed to have been incorporated at a constant rate since the time of burial. The previous works stated that correct ESR age of a sample lies always somewhere between the EU and LU uptake ages. In recent years, combined ESR/U-series methods are becoming known as a unique approach for dating old fossils directly, and were applied on several archaeological sites in the world. The archaeologists and dating specialists in China are called on to make a good joint effort and collaboration in installing and developing the combined ESR/U-series dating methods and to carry out better studies on chronology of Middle-Early Pleistocene sites.
分 类 号:P533[天文地球—古生物学与地层学]
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