The identification of Jurassic stratigraphy in southern Hainan Island: Evidence from detrital zircon U-Pb ages and Hf isotopic compositions

HU Zailong; WANG Yong; ZHAO Xiaoming; WEI Changxin; LIN Yihua; YUAN Haijun; MENG Zhongying; WU Nianwen

2019 Vol. 38, No. 10

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HU Zailong, WANG Yong, ZHAO Xiaoming, WEI Changxin, LIN Yihua, YUAN Haijun, MENG Zhongying, WU Nianwen. The identification of Jurassic stratigraphy in southern Hainan Island: Evidence from detrital zircon U-Pb ages and Hf isotopic compositions[J]. Geological Bulletin of China, 2019, 38(10): 1740-1757.

Citation:

HU Zailong, WANG Yong, ZHAO Xiaoming, WEI Changxin, LIN Yihua, YUAN Haijun, MENG Zhongying, WU Nianwen. The identification of Jurassic stratigraphy in southern Hainan Island: Evidence from detrital zircon U-Pb ages and Hf isotopic compositions[J]. Geological Bulletin of China, 2019, 38(10): 1740-1757.

The identification of Jurassic stratigraphy in southern Hainan Island: Evidence from detrital zircon U-Pb ages and Hf isotopic compositions

1.
Hainan Geological Survey Institute, Haikou 570206, Hainan, China
2.
School of Geosciences and Info-physics, Central South University, Changsha 410083, Hu'nan, China
3.
Wuhan Center of China Geological Survey, Wuhan 430223, Hubei, China

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Corresponding author: WANG Yong, wangyong5020@126.com

Received Date: 16 June 2019

Revised Date: 14 August 2019

Publish Date: 15 October 2019

Abstract

Abstract

The Hainan Island has long been considered as lacking the Jurassic deposition, which suggests that Hainan Island and interior continent have different Mesozoic evolutions. In this study, the authors conducted detrital zircon U-Pb analysis for the fuchsia clastic rocks in the Jianling and Hailuoling section and the Early Cretaceous Lumuwan Formation rocks, which are located at Sanya, southern Hainan. The zircon U-Pb dating results of the fuchsia clastic rocks from the two sections illustrate similar age spectra and oldest depositional age (172~174Ma). They are completely different from the spectrum of the underlying Late Ordovician Yuhong Formation and Early Cretaceous Lumuwan Formation samples. Together with previous tectonic and igneous activity records as well as the zircon Hf isotopic characteristics of the fuchsia clastic rocks, the authors hold that the deposition of the fuchsia clastic rocks in Jianling and Hailuoling must have occurred during 172~158Ma in the Middle-Late Jurassic periods. The sedimentary provenance and tectonic background were similar to those of the contemporary sedimentary rocks in eastern Guangdong and Fujian, indicating a uniform tectonic environment during the Middle-Late Jurassic in the southeast coastal area of South China.
- Hainan Island /
- Jurassic /
- detrital zircon /
- U-Pb chronology /
- Hf isotope

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References

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