| 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.
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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.
| Geology & Mineral Resources Departmentof Yunnan Province, 1990. Regional Geology of Yunnan Province. Geological Publishing House, Beijing. 493- 502(in Chinese) |
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| 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) |
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| 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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