Detrital zircons from Neoproterozoic sedimentary rocks in the Yili Block: Constraints on the affinity of microcontinents in the southern Central Asian Orogenic Belt
Detrital zircons from Neoproterozoic sedimentary rocks in the Yili Block: Constraints on the affinity of microcontinents in the southern Central Asian Orogenic Belt
Authors
Keywords
Yili Block, Detrital zircon, Crustal growth, Tectonic affinity, Central Asian Orogenic Belt
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