Detrital Zircon U-Pb Geochronology from Greywackes in the Niujuanzi Ophiolitic Mélange, Beishan Area, NW China: Provenance and Tectonic Implications

Shengdong Wang; Kexin Zhang; Bowen Song; Shucai Li; Jianxing Li; Jiyuan Yu; Jianjun Bu

doi:10.1007/s12583-018-0824-2

Volume 29 Issue 1

Jan 2018

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Journal of Earth Science > 2018 > 29(1): 103-113.

Shengdong Wang, Kexin Zhang, Bowen Song, Shucai Li, Jianxing Li, Jiyuan Yu, Jianjun Bu. Detrital Zircon U-Pb Geochronology from Greywackes in the Niujuanzi Ophiolitic Mélange, Beishan Area, NW China: Provenance and Tectonic Implications. Journal of Earth Science, 2018, 29(1): 103-113. doi: 10.1007/s12583-018-0824-2

Citation:

Shengdong Wang, Kexin Zhang, Bowen Song, Shucai Li, Jianxing Li, Jiyuan Yu, Jianjun Bu. Detrital Zircon U-Pb Geochronology from Greywackes in the Niujuanzi Ophiolitic Mélange, Beishan Area, NW China: Provenance and Tectonic Implications. Journal of Earth Science, 2018, 29(1): 103-113. doi: 10.1007/s12583-018-0824-2

Citation:

Shengdong Wang, Kexin Zhang, Bowen Song, Shucai Li, Jianxing Li, Jiyuan Yu, Jianjun Bu. Detrital Zircon U-Pb Geochronology from Greywackes in the Niujuanzi Ophiolitic Mélange, Beishan Area, NW China: Provenance and Tectonic Implications. Journal of Earth Science, 2018, 29(1): 103-113. doi: 10.1007/s12583-018-0824-2

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Detrital Zircon U-Pb Geochronology from Greywackes in the Niujuanzi Ophiolitic Mélange, Beishan Area, NW China: Provenance and Tectonic Implications

doi: 10.1007/s12583-018-0824-2

1.
Institute of Geophysical and Geochemical Exploration, Chinese Academy of Geological Sciences, Langfang 065000, China
2.
Institute of Geological Survey, China University of Geosciences, Wuhan 430074, China
3.
State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan 430074, China
4.
Cores and Samples Center of Land and Resources, China Geological Survey, Langfang 065201, China
5.
Xi'an Center of Geological Survey, Geological Survey of China, Xi'an 710000, China
6.
Wuhan Center of Geological Survey, Geological Survey of China, Wuhan 430205, China

More Information

Corresponding author: Kexin Zhang, kx_zhang@cug.edu.cn
Received Date: 30 Jun 2016
Accepted Date: 20 Mar 2017
Publish Date: 01 Feb 2018

Abstract

Abstract

The Niujuanzi ophiolitic mélange represents the remnant of oceanic crust between the Dunhuang massif and Mingshui-Hanshan massif. Greywacke from different tectonic slices in the Niujuanzi ophiolitic mélange were analyzed for detrital zircon U-Pb geochronology, trace elements and whole-rock trace elements to infer their provenance and the evolution of the Niujuanzi Ocean. Sample N-76s containing Carboniferous spores has the youngest zircon age of 323 Ma, while sample N-85s without fossils has the youngest zircon age of 449 Ma. The two samples were deposited no earlier than 323 and 449 Ma, respectively. The greywackes are depleted in large ion lithophile elements, and are relatively enriched in high field strength elements. The age spectra and trace element concentrations indicate that the sediments may have been deposited near the trench. The Hf, U, and Yb contents of zircons from sample N-76s vary widely, whereas those from sample N-85s have a narrow range. Sample N-76s contains both continental and oceanic zircons, while sample N-85s contains only continental zircons. The sediments were derived from the continental arc and accretionary wedge. The Paleozoic oceanic crust zircons have ages of 430–500 Ma, indicating the timing of the expansion of the Hongliuhe-Niujuanzi-Xichangjing Ocean expansion. The oldest Paleozoic continental zircon has an age of 470 Ma, suggesting that the northward subduction of the oceanic crust may have started at that time.
- detrital zircon,
- U-Pb geochronology,
- Niujuanzi ophiolitic mélange,
- Beishan

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Detrital Zircon U-Pb Geochronology from Greywackes in the Niujuanzi Ophiolitic Mélange, Beishan Area, NW China: Provenance and Tectonic Implications

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Detrital Zircon U-Pb Geochronology from Greywackes in the Niujuanzi Ophiolitic Mélange, Beishan Area, NW China: Provenance and Tectonic Implications

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