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    Ca. 825 Ma komatiitic basalts in South China: First evidence for >1500 degrees C mantle melts by a Rodinian mantle plume

    Ca. 825 Ma komatiitic basalts in South China: First evidence for >1500 degrees C mantle melts by a Rodinian mantle plume by Wang, X., Li, X., Li, W., Li, Zheng-Xiang

    Published 2007
    “…Mantle plume or superplume activities have repeatedly been invoked as a cause for the breakup of the Neoproterozoic supercontinent Rodinia, with supportive evidence including radiating dike swarms, globally synchronous anorogenic igneous activity, large-scale lithospheric doming and unroofing, and geochemical signatures similar to recent plume-related magmatism. …”
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