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HomeAdvanced Materials ResearchAdvanced Materials Research Vols. 734-737Formation Age of the Qinling Complex and the early...

Formation Age of the Qinling Complex and the early Paleozoic Tectonic Event

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Abstract:

The Qinling orogenic belt (QOB) located between the North China Craton (NCC) and the South China Craton (SCC) is composed of the Northern Qinling Belt (NQB) and the Southern Qinling Belt (SQB). This study presents new geochemical data, zircon U-Pb ages and Hf isotopes from two rocks from the Qinling complex in the NQB. LA-ICP-MS zircon U-Pb dating results suggest that the Qinling complex was formed in early Neoproterozoic and experienced the early Paleozoic metamorphism. High ε_Hf(t) values of 9.0-12.0 for the early Paleozoic zircons indicated that there is mantle-derived magma intruding into the Qinling complex in the early Paleozoic.

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Periodical:

Advanced Materials Research (Volumes 734-737)

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60-70

DOI:

https://doi.org/10.4028/www.scientific.net/AMR.734-737.60

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Online since:

August 2013

Authors:

Yu Shi*, Xi Jun Liu, Zuo Hai Feng

Keywords:

Geochemistry, Hf Isotopes, Qinling Complex, Zircon U-Pb Geochronology

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© 2013 Trans Tech Publications Ltd. All Rights Reserved

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