Formation Age and Evolution Time Span of the Koktokay No. 3 Pegmatite, Altai, NW China: Evidence from U-Pb Zircon and 40Ar-39Ar Muscovite Ages

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Formation Age and Evolution Time Span of the Koktokay No. 3 Pegmatite, Altai, NW China: Evidence from U-Pb Zircon and 40Ar-39Ar Muscovite Ages

© 2015 The Society of Resource Geology.The Koktokay No. 3 pegmatite is the largest Li-Be-Nb-Ta-Cs pegmatitic rare-metal deposit of the Chinese Altai orogenic belt, and is famous for its concentric ring zonation pattern (nine internal zones). However, the formation age and evolution time span have be...

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Bibliographic Details
Main Authors:	Zhou, Q., Qin, K., Tang, D., Tian, Y., Cao, Mingjian, Wang, C.
Format:	Journal Article
Published:	Society of Resource Geology 2015
Online Access:	http://hdl.handle.net/20.500.11937/52657

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