Whole-rock Nd–Hf isotopic study of I-type and peraluminous granitic rocks from the Chinese Altai: Constraints on the nature of the lower crust and tectonic setting
Whole-rock Nd–Hf isotopic study of I-type and peraluminous granitic rocks from the Chinese Altai: Constraints on the nature of the lower crust and tectonic setting
Authors
Keywords
Nd–Hf decoupling, Chinese Altai, Central Asian Orogenic Belt, Continental growth, Accretionary orogeny
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