滇西腾冲地块新生代火山岩中高温麻粒岩包体的发现及成因

林木森; 彭松柏; 乔卫涛; 李昌年; 徐海军

doi:10.3799/dqkx.2014.076

Volume 39 Issue 7

Jul. 2014

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Article Navigation > Earth Science > 2014 > 39(7): 807-819

Lin Musen, Peng Songbai, Qiao Weitao, Li Changnian, Xu Haijun, 2014. Characteristics and Genetic Significance of High Temperature Granulite Xenoliths in Cenozoic Volcanic Rocks, Tengchong, Western Yunnan Province, China. Earth Science, 39(7): 807-819. doi: 10.3799/dqkx.2014.076

Citation:

Lin Musen, Peng Songbai, Qiao Weitao, Li Changnian, Xu Haijun, 2014. Characteristics and Genetic Significance of High Temperature Granulite Xenoliths in Cenozoic Volcanic Rocks, Tengchong, Western Yunnan Province, China. Earth Science, 39(7): 807-819. doi: 10.3799/dqkx.2014.076

Citation:

Lin Musen, Peng Songbai, Qiao Weitao, Li Changnian, Xu Haijun, 2014. Characteristics and Genetic Significance of High Temperature Granulite Xenoliths in Cenozoic Volcanic Rocks, Tengchong, Western Yunnan Province, China. Earth Science, 39(7): 807-819. doi: 10.3799/dqkx.2014.076

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Characteristics and Genetic Significance of High Temperature Granulite Xenoliths in Cenozoic Volcanic Rocks, Tengchong, Western Yunnan Province, China

doi: 10.3799/dqkx.2014.076

1.
Faculty of Earth Sciences, China University of Geosciences, Wuhan 430074, China
2.
Three Gorges Research Center for Geo-hazards, Ministry of Education, China University of Geosciences, Wuhan 430074, China
3.
Guizhou Geological Survey, Guiyang 550004, China

Received Date: 2013-12-20
Publish Date: 2014-07-15

Abstract

Abstract

Researches on the Cenozoic volcanic rocks of the Mangbang Formation in the Mangbang area of the Tengchong block, South China, reveals many granulite xenoliths of felsic granulite and two-pyroxene granulite in trachyandesite. The granulite xenoliths range 3-5 cm in diameters, featured with aligned formation and blastic texture. Equilibrium temperature and pressure estimates for the felsic granulite xenoliths and two-pyroxene granulite xenoliths are 869-969 ℃, 0.94-1.00 GPa and 841-972 ℃ respectively, indicating that they are high temperature granulites. The crystallization temperature and pressure of trachyandesite phenocryst is 1 008-1 059 ℃, 1.26-1.33 GPa, indicating that they were formed in and originated from the lower crust to the top of the upper mantle. Electron backscatter diffraction(EBSD) analyses of two-pyroxene granulite xenoliths show that orthopyroxene and clinopyroxene have obvious lattice preferred orientation (LPO), and the main slip systems are: (010) [001] and (100) [001], (010) [001] respectively. The deformation mechanism is dislocation creep, which indicates that granulite xenoliths experienced a strong plastic deformation and metamorphism. The discovery of high temperature granulite in Cenozoic volcanic rocks suggests that Tengchong Cenozoic magmatic activity may be related with volcanic magamatism and high temperature metamorphism in the lower crustal caused by post-collisional extensional collapse, delamination and slab break-off after subduction and collision of the Indian Plate and the Tengchong block.
- Tengchong block,
- Cenozoic trachyandesite,
- High-temperature granulite xenolith,
- equilibrium temperature and pressure,
- electron backscatter diffraction,
- micro-fabric,
- petrology

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References(98)

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Characteristics and Genetic Significance of High Temperature Granulite Xenoliths in Cenozoic Volcanic Rocks, Tengchong, Western Yunnan Province, China

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