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Volume 15 Issue 2
Jun 2004
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Article Contents
Zhibin Zhang, Jing Li, Guxian Lü, Hua Yu, Fangzheng Wang. Characteristics of Blueschist in Shuangjiang Tectonic Mélange Zone, West Yunnan Province. Journal of Earth Science, 2004, 15(2): 224-231.
Citation: Zhibin Zhang, Jing Li, Guxian Lü, Hua Yu, Fangzheng Wang. Characteristics of Blueschist in Shuangjiang Tectonic Mélange Zone, West Yunnan Province. Journal of Earth Science, 2004, 15(2): 224-231.

Characteristics of Blueschist in Shuangjiang Tectonic Mélange Zone, West Yunnan Province

Funds:

the MajorScience and Technology Developing Program 2002201

the Ministry of Land and Resources, the National Natural Science Foundation of China 40372105

1∶ 250 000 Lincang County Regional Geological Survey 200013000150

  • Glaucophane in Shuangjiang area, West Yunnan Province, supplies a chance for studying south segment of Lancangjiang tectonic zone. But people are at odds as to whether two-stage glaucophane exists or not, glaucophane is the result of dynamic metamorphism later, or indicates a high P/T metamorphic belt when Paleozoic Tethys Sea closed. Authors discover in a recent research that there is only one-stage glaucophane in Shuangjiang area, and three blueschist belts are distributed near N-S-tending, and glaucophane in Shuangjiang area is related to the eastward subduction of ChangningMenglian basin.

     

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  • Geology & Mineral Resources Departmentof Yunnan Province, 1990. Regional Geology of Yunnan Province. Geological Publishing House, Beijing. 493- 502(in Chinese)
    Peng, X. J., Luo, W. L., 1982. The Discovery and Earth Tectonic Significance of the Blueschist Belt in Lancangjiang South Segment of West Yunnan. Regional Geology of China, (2): 69- 75(in Chinese with English Abstract)
    Xue, X. H., Xiong, J. R., et al., 1989. Yunnan Metamorphic Complex(the Explanation of Metamorphic Map of Yunnan Province on the Scale of 1∶2 000 000). Tech-Science Press of Yunnan Province, Kunming(in Chinese)
    Zhao, J., Zhong, D. L., 1994a. Metamorphism of Lancang Metamorphic Belt, the Western Yunnan and Its Relation to Deformation. Acta Petrologica Sinica, 10(1): 27- 40(in Chinese with English Abstract)
    Zhao, J., Zhong, D. L., 1994b. APreliminary Study on Deformation Sequence and Metamorphism in LancangMetamorphic Belt of West Yunnan. Scientia Geologica Sinica, 29(4): 366- 372 (in Chinese with English Abstract)
    Zhao, J., 1993, A Study of Muscovites from the Lancang Metamorphic Belt in Western Yunnan and Its Geological Significance. Acta Petrologica et Mineralogica, 12(3): 251- 260(in Chinese with English Abstract)
    Zhong, D. L., 1998. Orogene of Paleo-Tethys in West Yunnan and Sichuan. Science Press, Beijing. 173- 178(in Chinese)
    Zhou, W.Q., Lin, W. X., 1982. Characteristics of Blueschist the South Segmentof LancangMetamorphic Belt. Regional Geology of China, (2): 76- 85(in Chinese with English Abstract)
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