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Volume 20 Issue 6
Dec 2009
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Article Contents
Dapeng Li, Yuelong Chen, Zhaohua Luo, Junxiang Zhao. Zircon SHRIMP U-Pb dating and neoproterozoic metamorphism of Kangding and Yuanmou intrusive complexes, Sichuan and Yunnan. Journal of Earth Science, 2009, 20(6): 897-908. doi: 10.1007/s12583-009-0076-2
Citation: Dapeng Li, Yuelong Chen, Zhaohua Luo, Junxiang Zhao. Zircon SHRIMP U-Pb dating and neoproterozoic metamorphism of Kangding and Yuanmou intrusive complexes, Sichuan and Yunnan. Journal of Earth Science, 2009, 20(6): 897-908. doi: 10.1007/s12583-009-0076-2

Zircon SHRIMP U-Pb dating and neoproterozoic metamorphism of Kangding and Yuanmou intrusive complexes, Sichuan and Yunnan

doi: 10.1007/s12583-009-0076-2
Funds:

the National Natural Science Foundation of China 40673046

the National Natural Science Foundation of China 40173007

the National Natural Science Foundation of China 40234052

Key Project of the Ministry of Education Key 03032

More Information
  • Corresponding author: Chen Yuelong , chyl@cugb.edu.cn
  • Received Date: 10 Dec 2008
  • Accepted Date: 30 May 2009
  • To clarify the relationship of the metamorphic intrusions along the west margin of the Yangtze craton and their metamorphic history after crystallization, the petrochemical and trace element geochemical characters, zircon SHRIMP U-Pb dating, and the chemical compositions of coexisting hornblendes and plagioclases from Neoproterozoic metamorphic intrusions in Kangding (康定), Sichuan (四川) Province, and Yuanmou (元谋), Yunnan (云南) Province, were studied. Combined with the former published data, it is indicated that the Kangding granitic plutons and Yuanmou complex in the west margin of the Yangtze craton generally formed at the same period. Metamorphic event at ~700 Ma existed extensively, at least covering from Kangding area in Sichuan to the Eshan (峨山) area in Central Yunnan. Moreover, amphibolite facies may represent the peak regional metamorphic condition.

     

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