内蒙乌拉特中旗图古日格二叠纪角闪石岩年龄、岩石成因及构造背景

王键; 孙丰月; 李碧乐; 王英德; 李睿华

doi:10.3799/dqkx.2016.067

Volume 41 Issue 5

May 2016

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Article Navigation > Earth Science > 2016 > 41(5): 792-808

Wang Jian, Sun Fengyue, Li Bile, Wang Yingde, Li Ruihua, 2016. Age, Petrogenesis and Tectonic Implications of Permian Hornblendite in Tugurige, Urad Zhongqi, Inner Mongolia. Earth Science, 41(5): 792-808. doi: 10.3799/dqkx.2016.067

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Wang Jian, Sun Fengyue, Li Bile, Wang Yingde, Li Ruihua, 2016. Age, Petrogenesis and Tectonic Implications of Permian Hornblendite in Tugurige, Urad Zhongqi, Inner Mongolia. Earth Science, 41(5): 792-808. doi: 10.3799/dqkx.2016.067

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Age, Petrogenesis and Tectonic Implications of Permian Hornblendite in Tugurige, Urad Zhongqi, Inner Mongolia

doi: 10.3799/dqkx.2016.067

College of Earth Sciences, Jilin University, Changchun 130061, China

Received Date: 2016-02-26
Publish Date: 2016-05-15

Abstract

Abstract

Electron microprobe results, zircon U-Pb dating, Hf isotope data and geochemistry of hornblendite at Tugurige, Urad Zhongqi, Inner Mongolia are reported in the paper, which provide constraints on formation time, magma source, and tectonic setting of the intrusions. The dating results indicate that the hornblendite formed in the late Early Permian (273.5±1.3 Ma, MSWD=0.48; 274.4±4.3 Ma, MSWD=0.041), and it contains low Na₂O and K₂O, high Al₂O₃, TFe₂O₃, MgO, CaO, Mg^#=46.95-63.53, M/F=0.87-1.72. Chondrite-normalized REE patterns show LREE enrichment. On a trace element spider diagram, large ion lithophile elements (LILEs) such as Rb, Ba and K are enriched, whereas the high field strength elements Ti, P, Th and U are relatively depleted. Electronic Probe analysis results show that hornblende belongs to calcic amphibole and has the characteristics of mantle hornblende. The ε _Hf(t) values of zircons from the hornblendite vary between -0.3 and 8.5, and their Hf one-stage model ages vary from 580 to 920 Ma, implying that their magma source was derived from a depleted mantle and may have been added metasomatic enriched lithospheric mantle components. Combined with regional tectonic evolution, the hornblendite formed in the post-collisional extension setting, perhaps triggered by slab break-off.
- Inner Mongolia,
- Urad Zhongqi,
- crystal chemistry,
- geochronology,
- geochemistry,
- Hf isotope

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References(102)

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Age, Petrogenesis and Tectonic Implications of Permian Hornblendite in Tugurige, Urad Zhongqi, Inner Mongolia

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