西秦岭北缘秦岭杂岩变质作用:副片麻岩岩石学、相平衡模拟及其地质意义

毛小红; 张建新; 于胜尧; 李云帅; 喻星星; 路增龙; 周桂生

doi:10.3799/dqkx.2018.017

Volume 43 Issue 1

Jan. 2018

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Article Navigation > Earth Science > 2018 > 43(1): 278-295

Mao Xiaohong, Zhang Jianxin, Yu Shengyao, Li Yunshuai, Yu Xingxing, Lu Zenglong, Zhou Guisheng, 2018. Metamorphism of Qinling Complex in Northern West Qinling Orogen: Petrology, Phase Equilibria Modelling of Paragneiss and Their Geological Implication. Earth Science, 43(1): 278-295. doi: 10.3799/dqkx.2018.017

Citation:

Mao Xiaohong, Zhang Jianxin, Yu Shengyao, Li Yunshuai, Yu Xingxing, Lu Zenglong, Zhou Guisheng, 2018. Metamorphism of Qinling Complex in Northern West Qinling Orogen: Petrology, Phase Equilibria Modelling of Paragneiss and Their Geological Implication. Earth Science, 43(1): 278-295. doi: 10.3799/dqkx.2018.017

Citation:

Mao Xiaohong, Zhang Jianxin, Yu Shengyao, Li Yunshuai, Yu Xingxing, Lu Zenglong, Zhou Guisheng, 2018. Metamorphism of Qinling Complex in Northern West Qinling Orogen: Petrology, Phase Equilibria Modelling of Paragneiss and Their Geological Implication. Earth Science, 43(1): 278-295. doi: 10.3799/dqkx.2018.017

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Metamorphism of Qinling Complex in Northern West Qinling Orogen: Petrology, Phase Equilibria Modelling of Paragneiss and Their Geological Implication

doi: 10.3799/dqkx.2018.017

1.
Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China
2.
School of Earth and Space Sciences, Peking University, Beijing 100871, China
3.
Key Lab of Submarine Geosciences and Prospecting Techniques, Minstry of Education; College of Marine Geosciences, Ocean University of China, Qingdao 266100, China
4.
Laboratory for Marine Geology, Qingdao National Laboratory for Marine Science and Technology, Qingdao 266235, China
5.
Institute of Surface-Earth System Science, Tianjin University, Tianjin 300072, China

Received Date: 2017-09-24
Publish Date: 2018-01-15

Abstract

Abstract

Studies of high-grade metamorphic rocks in an ancient orogenic belt can provide important constraints on the formation and tectonic evolution of orogen. The Qinling complex in the northern West Qinling orogen mainly consists of orogneiss, paragneiss, minor metabasite (mafic granulite) and marble. The petrography, mineral chemistry and phase equilibria modelling in this study show that paragneiss has experencied three metamorphic evolution stages. Stage 1 is the prograde stage, characterized by biotite and quartz occurring as inclusions in garnet. Stage 2 is the peak metamorphic stage, and mineral assemblage in this stage is interpreted to be garnet+sillimanite+K-feldspar+plagioclase+biotite+quartz+rutile, which formed in P-T conditions of 793-803℃ and 8.8-9.5 kbar. Stage 3 is the retrograde stage with decrease in temperature and pressure, which is recorded by garnet and plagioclase. Combining with previous data, it is suggested that the Qinling complex in the northern West Qinling orogen has experienced Early Paleozoic metamorphism and anataxis related to collision orogenesis.
- West Qinling,
- Qinling complex,
- paragneiss,
- metamorphism,
- phase equilibria modelling,
- petrology

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References(110)

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Metamorphism of Qinling Complex in Northern West Qinling Orogen: Petrology, Phase Equilibria Modelling of Paragneiss and Their Geological Implication

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