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    P-T-t evolution of pelitic gneiss from the basement underlying the Northwestern Ordos Basin, North China Craton, and the tectonic implications

    P-T-t evolution of pelitic gneiss from the basement underlying the Northwestern Ordos Basin, North China Craton, and the tectonic implications by Gou, Long-Long, Zhang, C., Brown, M., Piccoli, P., Lin, H., Wei, X.

    Published 2016
    “…Together with the occurrence of mid-Paleoproterozoic magmatism in the basement of the Ordos Basin, these features indicate that the Ordos Terrane was the upper plate at a convergent margin with the Khondalite Belt representing the forearc sediments along its northern edge. …”
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