Early Paleoproterozoic Oceanic Subduction in the Southern Margin of North China Craton: Constraints from Zircon U–Pb Geochronology, Geochemistry and Sr-Nd-Hf Isotopes of ca. 2.3 Ga Mafic Intrusions | Zendy

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Early Paleoproterozoic Oceanic Subduction in the Southern Margin of North China Craton: Constraints from Zircon U–Pb Geochronology, Geochemistry and Sr-Nd-Hf Isotopes of ca. 2.3 Ga Mafic Intrusions

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