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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，金沙江蛇綠混襍巖具有相對較高的~(208)Pb/~(204)Pb和~(207)Pb/~(204)Pb，顯示了具有DUPAL異常型的特征，類似於古特提斯的地幔特征。
• Dupal anomaly
  Dupal異常
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