东秦岭商丹地区刘岭群浅变质沉积岩系碎屑锆石U-Pb年龄及其地质意义

高峰; 裴先治; 李瑞保; 李佐臣; 裴磊; 陈有炘; 王盟; 刘成军; 李宗耀

doi:10.3799/dqkx.2018.164

Volume 44 Issue 7

Jul. 2019

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Article Navigation > Earth Science > 2019 > 44(7): 2519-2531

Gao Feng, Pei Xianzhi, Li Ruibao, Li Zuochen, Pei Lei, Chen Youxin, Wang Meng, Liu Chengjun, Li Zongyao, 2019. Detrital Zircon U-Pb Ages and Geological Significance of Low-Metamorphosed Liuling Sedimentary Assemblage in the Shangdan Area, Eastern Qinling Orogenic Belt. Earth Science, 44(7): 2519-2531. doi: 10.3799/dqkx.2018.164

Citation:

Gao Feng, Pei Xianzhi, Li Ruibao, Li Zuochen, Pei Lei, Chen Youxin, Wang Meng, Liu Chengjun, Li Zongyao, 2019. Detrital Zircon U-Pb Ages and Geological Significance of Low-Metamorphosed Liuling Sedimentary Assemblage in the Shangdan Area, Eastern Qinling Orogenic Belt. Earth Science, 44(7): 2519-2531. doi: 10.3799/dqkx.2018.164

Citation:

Gao Feng, Pei Xianzhi, Li Ruibao, Li Zuochen, Pei Lei, Chen Youxin, Wang Meng, Liu Chengjun, Li Zongyao, 2019. Detrital Zircon U-Pb Ages and Geological Significance of Low-Metamorphosed Liuling Sedimentary Assemblage in the Shangdan Area, Eastern Qinling Orogenic Belt. Earth Science, 44(7): 2519-2531. doi: 10.3799/dqkx.2018.164

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Detrital Zircon U-Pb Ages and Geological Significance of Low-Metamorphosed Liuling Sedimentary Assemblage in the Shangdan Area, Eastern Qinling Orogenic Belt

doi: 10.3799/dqkx.2018.164

Gao Feng^1
,,
Pei Xianzhi^{1,2
,
,},
Li Ruibao^1,2,
Li Zuochen^1,2,
Pei Lei^1,2,
Chen Youxin^1,2,
Wang Meng^1,2,
Liu Chengjun^1,2,
Li Zongyao¹

1.
School of Earth Science and Resources, Chang'an University, Xi'an 710054, China
2.
Key Laboratory for the Study of Focused Magmatism and Giant Ore Deposits, MNR, Xi'an 710054, China

Received Date: 2018-04-03
Publish Date: 2019-07-15

Abstract

Abstract

The conventional Liuling Group is widespread in the northern part of South Qinling structure zone, which has been regarded as a key factor for revealing the convergence process between South Qinling structure zone and North Qinling structure zone in Early Paleozoic for its significant tectonic position. Compared to the Liuling Group exposed in Shanyang-Zhashui area, Liuling Group in Danfeng-Shangnan-Xiping area is more complicated in the degree of deformation and metamorphism, which is named as low-metamorphosed Liuling sedimentary assemblage and Liuling sedimentary assemblage in this paper, respectively.Liuling sedimentary assemblage in Shanyang-Zhashui area was defined as Middle-Upper Devonian based on reliable fossils, while there are none fossil evidences for low-metamorphosed Liuling sedimentary assemblage, defined as Lower Paleozoic.In this paper, LA-ICP-MS detrital zircon U-Pb ages of two garnet-bearing two-mica quartz schist samples in low-metamorphosed Liuling sedimentary assemblage were tested, results ranged from 2 598-390 Ma, yield two prominent age clusters at~1.0-0.6 Ga and~0.5-0.4 Ga, as well as three sub-prominent age clusters at~2.6-2.3 Ga, ~1.71-1.60 Ga and~1.3-1.2 Ga.Combined with regional geology, we suggest that:the Liuling sedimentary assemblage and low-metamorphosed Liuling sedimentary assemblage were mainly fed by South Qinling structure zone and North Qinling structure zone, own double-direction sources, they may have deposited at the same time in a forland basin, and experienced different degree of deformation and metamorphism lately.The maximum depositional age of low-metamorphosed Liuling sedimentary assemblage is~390 Ma, which most likely deposited in Middle-Late Devonian.
- Shangdan area in East Qinling,
- low-metamorphosed Liuling sedimentary assemblage,
- detrital zircon U-Pb ages,
- geochemistry

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Detrital Zircon U-Pb Ages and Geological Significance of Low-Metamorphosed Liuling Sedimentary Assemblage in the Shangdan Area, Eastern Qinling Orogenic Belt

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