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- The Pb isotopic features of the Jinshajiang ophiolitic melange display higher 208Pb/204Pb and 207Pb/204Pb ratios,implying a DUPAL anomaly,i. e. mantle signatures of Paleo-tethys.
Pb同位素研究表明,金沙江蛇绿混杂岩具有相对较高的~(208)Pb/~(204)Pb和~(207)Pb/~(204)Pb,显示了具有DUPAL异常型的特征,类似于古特提斯的地幔特征。 - Dupal anomaly
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