The relationship between Lincang block and provenance of Nanduan Formation:Evidence of detrital zircon U-Pb dating from metasandstone of Devonian-Carboniferous Nanduan Formation

ZENG Wentao; LIU Guichun; FENG Qinglai; ZHAO Tianyu; YU Saiying; DENG Renhong; MO Xiong

2017 Vol. 36, No. 7

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ZENG Wentao, LIU Guichun, FENG Qinglai, ZHAO Tianyu, YU Saiying, DENG Renhong, MO Xiong. The relationship between Lincang block and provenance of Nanduan Formation:Evidence of detrital zircon U-Pb dating from metasandstone of Devonian-Carboniferous Nanduan Formation[J]. Geological Bulletin of China, 2017, 36(7): 1175-1187.

Citation:

ZENG Wentao, LIU Guichun, FENG Qinglai, ZHAO Tianyu, YU Saiying, DENG Renhong, MO Xiong. The relationship between Lincang block and provenance of Nanduan Formation:Evidence of detrital zircon U-Pb dating from metasandstone of Devonian-Carboniferous Nanduan Formation[J]. Geological Bulletin of China, 2017, 36(7): 1175-1187.

The relationship between Lincang block and provenance of Nanduan Formation:Evidence of detrital zircon U-Pb dating from metasandstone of Devonian-Carboniferous Nanduan Formation

1.
Yunnan Institute of Geological Survey, Kunming 650216, Yunnan, China
2.
State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Wuhan 430074, Hubei, China

More Information

Corresponding author: FENG Qinglai, qinglaifeng@cug.edu.cn

Received Date: 01 December 2016

Revised Date: 09 June 2017

Publish Date: 25 July 2017

Abstract

Abstract

U-Pb ages of detrital zircons of Devonian-Carboniferous Nanduan Formation from Lincang block define three distinctive age peaks in older Grenvillian (1100~1300Ma), younger Grenvillian (900~980Ma) and Pan-African (530~680Ma), and two subordinate group in 1550~1730Ma and 2350~2630Ma, suggesting that the provenance of sediments had multi-source and complex characteristics. The age spectrum is obviously different from detrital zircon age spectrum of the Devonian-Carboniferous sediments of Simao block, which indicates that the sediments of Nanduan Formation came from East Ganwana supercontinent, and the result is indicated by paleobiology which shows a genetic relationship between East Ganwana and paleo-Tethys in southwest Yunnan.
- detrital zircon /
- LA-ICP-MS U-Pb age /
- provenance analysis /
- metasandstone /
- Nanduan Formation /
- Lincang block /
- southwest Yunnan

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References

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