Contrasting zircon Hf and O isotopes in the two episodes of Neoproterozoic granitoids in South China: Implications for growth and reworking of continental crust

Contrasting zircon Hf and O isotopes in the two episodes of Neoproterozoic granitoids in South China: Implications for growth and reworking of continental crust

The genetic links among rift magmatism, crustal growth and water–rock interaction are an important issue about mass and heat transfer betweenmantle and crust during supercontinent breakup.Acombined study ofHf andOisotopes in zircons fromNeoproterozoic granitoids in South China provides evidence for...

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Bibliographic Details
Main Authors: Zheng, Y., Zhang, S., Zhao, Z., Wu, Y., Li, X., Li, Zheng-Xiang, Wu, F.
Format: Journal Article
Published: Elsevier Science BV 2007
Subjects:
Neoproterozoic magmatism
O isotope
Mantle upwelling
South China
Continental growth
Zircon
Supercontinent breakup
Hf isotope
Online Access:http://hdl.handle.net/20.500.11937/21362

Internet

http://hdl.handle.net/20.500.11937/21362

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