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Petrogenesis of Late Cenozoic basaltic rocks from southern Vietnam
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文摘
The Vietnam basalts have Sr–Nd–Hf–Pb isotopic compositions defining a DMM-EM2 array. The Nd and Hf isotopic compositions are coupled and plot along the mantle–crust array. The enriched mantle component is likely to reside in the sub-lithosphere. They may be produced by the Hainan plume from recycled eclogitic oceanic crust.

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