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The tectonic–thermal history of the Huarong granitoids is used to clarify the tectonic evolution of the middle Yangtze Craton and eastern China. The Huarong granitoids include the Xiaomoshan and Taohuashan plutons and form a northeast-trending belt in the middle Yangtze Craton, eastern China. Multi-method geochronology reveals the thermal history of the Huarong granitoids from their emplacement to...
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