Detrital Zircon Geochronology of the Radial Sand Ridge System of Jiangsu Coast, East China: Implication for Sediment Provenance

Jinbao Su; Wenbo Rao; Yigang Wang; Changping Mao

doi:10.1007/s12583-017-0769-x

Volume 29 Issue 1

Jan 2018

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Journal of Earth Science > 2018 > 29(1): 144-154.

Jinbao Su, Wenbo Rao, Yigang Wang, Changping Mao. Detrital Zircon Geochronology of the Radial Sand Ridge System of Jiangsu Coast, East China: Implication for Sediment Provenance. Journal of Earth Science, 2018, 29(1): 144-154. doi: 10.1007/s12583-017-0769-x

Citation:

Jinbao Su, Wenbo Rao, Yigang Wang, Changping Mao. Detrital Zircon Geochronology of the Radial Sand Ridge System of Jiangsu Coast, East China: Implication for Sediment Provenance. Journal of Earth Science, 2018, 29(1): 144-154. doi: 10.1007/s12583-017-0769-x

Citation:

Jinbao Su, Wenbo Rao, Yigang Wang, Changping Mao. Detrital Zircon Geochronology of the Radial Sand Ridge System of Jiangsu Coast, East China: Implication for Sediment Provenance. Journal of Earth Science, 2018, 29(1): 144-154. doi: 10.1007/s12583-017-0769-x

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Detrital Zircon Geochronology of the Radial Sand Ridge System of Jiangsu Coast, East China: Implication for Sediment Provenance

doi: 10.1007/s12583-017-0769-x

1.
School of Earth Sciences and Engineering, Hohai University, Nanjing 210098, China
2.
School of Harbour, Coastal and Offshore Engineering, Hohai University, Nanjing 210098, China

More Information

Corresponding author: Wenbo Rao, raowenbo@163.com
Received Date: 11 Apr 2015
Accepted Date: 15 Jan 2016
Publish Date: 01 Feb 2018

Abstract

Abstract

The radial sand ridge system (RSRS) located at Jiangsu coast of China attracts much attention on its origin and mechanic of formation for its special structure and potential land resource. Due to complicated hydrodynamic condition, the Jiangsu RSRS is a hot debated on its potential sources, Yangtze River or Yellow River? We collected ten sand samples from surface sediments along the west coast of Bohai Sea and Yellow Sea from the modern Yellow River estuary to Yangtze River estuary in summer, 2013. The samples are analyzed by method of detrital zircon age for source identification of the RSRS sediments. The U-Pb age spectra of detrital zircon grains of the samples show a wide range from Cenozoic to Late Archean with several age peaks. Comparing the age spectra between the Yangtze River and the Yellow River, the detrital zircons have younger age (< 100 Ma) group in the Yangtze River. These age distribution of the Jiangsu coastal RSRS sediments are similar to that of the Yangtze River, but different from the Yellow River. The samples located adjacent to the old Yellow River Delta show more wide-range age distribution, implying a compounded origination from the both rivers. Based on these findings it is proposed that, contrary to common opinion, the main sediment source of the Jiangsu RSRS is the Yangtze River, rather than the Yellow River. By implication, there should be evidence of hydrodynamic mechanics of oceanic currents and tidal motion. This aspect awaits confirmation in future research.
- Yellow Sea,
- Jiangsu coast,
- radial sand ridge,
- zircon geochronology,
- sediment provenance

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Detrital Zircon Geochronology of the Radial Sand Ridge System of Jiangsu Coast, East China: Implication for Sediment Provenance

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Detrital Zircon Geochronology of the Radial Sand Ridge System of Jiangsu Coast, East China: Implication for Sediment Provenance

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