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本文对西藏当雄和羊八井三个泥炭和腐植质层样品的 C~(14)同位素地质年龄测定的结果作简要报导,并讨论其地质意义。样品采集点的地理位置见图1。
In this paper, the results of the C ~ (14) isotopic geochronological dating of three peat and humus samples in the Dangxiong and Yangbajing of Tibet are briefly reported, and their geological implications are discussed. The location of the sample collection point is shown in Figure 1.