桐柏造山带中龟山杂岩的白云母<sup>40</sup>Ar/<sup>39</sup>Ar年龄及其地质意义

曲玮; 刘晓春; 崔建军; 胡娟; 李淼

doi:10.3799/dqkx.2018.015

Volume 43 Issue 1

Jan. 2018

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Article Navigation > Earth Science > 2018 > 43(1): 247-258

Qu Wei, Liu Xiaochun, Cui Jianjun, Hu Juan, Li Miao, 2018. 40Ar/39Ar Dating of Muscovite from the Guishan Complex in the Tongbai Orogen, Central China, and Its Geological Implications. Earth Science, 43(1): 247-258. doi: 10.3799/dqkx.2018.015

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Qu Wei, Liu Xiaochun, Cui Jianjun, Hu Juan, Li Miao, 2018. ⁴⁰Ar/³⁹Ar Dating of Muscovite from the Guishan Complex in the Tongbai Orogen, Central China, and Its Geological Implications. Earth Science, 43(1): 247-258. doi: 10.3799/dqkx.2018.015

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⁴⁰Ar/³⁹Ar Dating of Muscovite from the Guishan Complex in the Tongbai Orogen, Central China, and Its Geological Implications

doi: 10.3799/dqkx.2018.015

Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081, China

Received Date: 2017-09-03
Publish Date: 2018-01-15

Abstract

Abstract

The Guishan complex exposed to the south of the Songpa-Guimei fault in the Tongbai orogen underwent two-stage metamorphism and multiple deformation. However, the timing of metamorphism and deformation of the complex and its relation to the Wuguan complex occurring in the same tectonic position in the Qinling orogen remain poorly constrained. In this paper, 4 metasedimentary rocks and 2 metavolcanic rocks from the Guishan complex were performed for muscovite ⁴⁰Ar/³⁹Ar dating. The results suggest that the plateau ages of muscovite range from 306.7±1.7 Ma (well-preserved muscovite porphyroblasts) to 279.2±2.6 Ma (muscovites overprinted by late deformation). Coupled with published U-Pb zircon data, it is infered that two-stage metamorphism and main thrust deformation of the Guishan complex took place during the Carboniferous, and the reworking of sinistral slid-slip shearing occurred in the Permian. The Guishan and Wuguan complexes have similar rock associations and share the same metamorphic and deformational history. The two complexes constitute a >500 km-long Late Paleozoic medium-grade metamorphic belt, which was resulted from the oceanic subduction-accretion prior to the final collision between the North and South China blocks.
- Tongbai orogen,
- Guishan complex,
- ⁴⁰Ar/³⁹Ar dating,
- Late Paleozoic,
- petrology

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References(63)

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