云开地块东缘寒武系-泥盆系不整合界面上下的碎屑锆石U-Pb年代学记录及对物源转换的响应

王志宏; 杨文强; 周岱; 牛志军; 何垚砚; 宋芳

doi:10.3799/dqkx.2018.242

Volume 43 Issue 11

Nov. 2018

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Article Navigation > Earth Science > 2018 > 43(11): 4193-4203

Wang Zhihong, Yang Wenqiang, Zhou Dai, Niu Zhijun, He Yaoyan, Song Fang, 2018. Detrital Zircon U-Pb Geochronological Records and Its Response of Provenance Transformation of Strata Surrounding Cambrian-Devonian Unconformity in Eastern Margin of Yunkai Massif. Earth Science, 43(11): 4193-4203. doi: 10.3799/dqkx.2018.242

Citation:

Wang Zhihong, Yang Wenqiang, Zhou Dai, Niu Zhijun, He Yaoyan, Song Fang, 2018. Detrital Zircon U-Pb Geochronological Records and Its Response of Provenance Transformation of Strata Surrounding Cambrian-Devonian Unconformity in Eastern Margin of Yunkai Massif. Earth Science, 43(11): 4193-4203. doi: 10.3799/dqkx.2018.242

Citation:

Wang Zhihong, Yang Wenqiang, Zhou Dai, Niu Zhijun, He Yaoyan, Song Fang, 2018. Detrital Zircon U-Pb Geochronological Records and Its Response of Provenance Transformation of Strata Surrounding Cambrian-Devonian Unconformity in Eastern Margin of Yunkai Massif. Earth Science, 43(11): 4193-4203. doi: 10.3799/dqkx.2018.242

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Detrital Zircon U-Pb Geochronological Records and Its Response of Provenance Transformation of Strata Surrounding Cambrian-Devonian Unconformity in Eastern Margin of Yunkai Massif

doi: 10.3799/dqkx.2018.242

Wang Zhihong^{1,2
,},
Yang Wenqiang^1,2,
Zhou Dai¹,
Niu Zhijun^1,2,
He Yaoyan^2,3,
Song Fang^1,2

1.
Wuhan Center of China Geological Survey, Wuhan 430205, China
2.
Key Laboratory for Paleontology and Coevolution of Life and Environment, China Geological Survey, Wuhan 430205, China
3.
Institute of Geological Survey, China University of Geosciences, Wuhan 430074, China

Received Date: 2018-08-12
Publish Date: 2018-11-15

Abstract

Abstract

The unconformity of the Cambrian in the eastern margin of the Yunkai massif near Guigang, West Guangdong covers a set of gray-white quartz conglomerate-gravel sandstones. Due to the lack of fossils and U-Pb dating, the age of the stratum has remained controversial for a long time. By LA-ICP-MS U-Pb dating, a total of 300 valid data were obtained from 4 samples with age ranging from 2 900-400 Ma in this study. The samples below the unconformity surface are mainly concentrated at 1 100-700 Ma, and the youngest detrital zircon ages above the unconformity surface are concentrated at 450-400 Ma. The new dating data combined with previous research show that the ages of underlying and overlying strata in Guigang are Cambrian and Devonian, respectively. The source characteristics of the Cambrian are similar to those of the orogenic zone among India, eastern Antarctica and Australia. While the Devonian sources are relatively homogeneous, derived from the adjoining Yunkai massif. It is proposed that the unconformity of the study area should have resulted from the superposition of the Yu'nan orogeny and the Guangxi orogeny.
- Yunkai massif,
- detrital zircon,
- Yu'nan orogeny,
- Guangxi orogeny,
- geochronology,
- sedimentology

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References(52)

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Detrital Zircon U-Pb Geochronological Records and Its Response of Provenance Transformation of Strata Surrounding Cambrian-Devonian Unconformity in Eastern Margin of Yunkai Massif

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