2004: Recognition of Neoproterozoic ophiolite on the northern margin of the Qaidam basin: evidence of the breakup of Rodinia?. Geological Bulletin of China, 23(9): 892-898. DOI: 10.12097/gbc.200409160
    Citation: 2004: Recognition of Neoproterozoic ophiolite on the northern margin of the Qaidam basin: evidence of the breakup of Rodinia?. Geological Bulletin of China, 23(9): 892-898. DOI: 10.12097/gbc.200409160

    Recognition of Neoproterozoic ophiolite on the northern margin of the Qaidam basin: evidence of the breakup of Rodinia?

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