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Widespread Neoarchean (~ 2.7-2.6 Ga) magmatism of the Yangtze craton, South China, as revealed by modern river detrital zircons
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文摘
River detrital zircons reveal the formation history of the North Kongling Terrane. The 2.7–2.6 Ga magmatism formed most of the granitic crust in this terrane. The coeval tectono-thermal event(s) was also widespread in Yangtze. The event may correspond to the initial stabilization of the Yangtze craton.

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