扬子陆块三峡地区莲沱组砂岩中碎屑锆石U-Pb年龄、Hf同位素组成及其地质意义

徐琼; 江拓; 侯林春; 赵小明; 童喜润; 散飞雪; 邱啸飞

doi:10.3799/dqkx.2020.168

Volume 46 Issue 4

Apr. 2021

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Xu Qiong, Jiang Tuo, Hou Linchun, Zhao Xiaoming, Tong Xirun, San Feixue, Qiu Xiaofei, 2021. Detrital Zircon Compositions of U-Pb Ages and Hf Isotope for Sandstone of Liantuo Formation from Three Gorges Area, Yangtze Block and Its Geological Significance. Earth Science, 46(4): 1217-1230. doi: 10.3799/dqkx.2020.168

Citation:

Xu Qiong, Jiang Tuo, Hou Linchun, Zhao Xiaoming, Tong Xirun, San Feixue, Qiu Xiaofei, 2021. Detrital Zircon Compositions of U-Pb Ages and Hf Isotope for Sandstone of Liantuo Formation from Three Gorges Area, Yangtze Block and Its Geological Significance. Earth Science, 46(4): 1217-1230. doi: 10.3799/dqkx.2020.168

Citation:

Xu Qiong, Jiang Tuo, Hou Linchun, Zhao Xiaoming, Tong Xirun, San Feixue, Qiu Xiaofei, 2021. Detrital Zircon Compositions of U-Pb Ages and Hf Isotope for Sandstone of Liantuo Formation from Three Gorges Area, Yangtze Block and Its Geological Significance. Earth Science, 46(4): 1217-1230. doi: 10.3799/dqkx.2020.168

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Detrital Zircon Compositions of U-Pb Ages and Hf Isotope for Sandstone of Liantuo Formation from Three Gorges Area, Yangtze Block and Its Geological Significance

doi: 10.3799/dqkx.2020.168

Xu Qiong^{1, 2, 3
,
,},
Jiang Tuo¹,
Hou Linchun⁴,
Zhao Xiaoming^{1, 3},
Tong Xirun¹,
San Feixue⁵,
Qiu Xiaofei^{1, 2, 3
,
,
,}

1.
Wuhan Center of China Geological Survey, Wuhan 430205, China
2.
Institute of Geological Survey, China University of Geosciences, Wuhan 430074, China
3.
Hubei Key Laboratory of Paleontology and Geological Environment Evolution, Wuhan 430205, China
4.
School of Geography and Information Engineering, China University of Geosciences, Wuhan 430074, China
5.
School of Earth Sciences, China University of Geosciences, Wuhan 430074, China

Received Date: 2020-04-15
Publish Date: 2021-04-15

Abstract

Abstract

In this study, 120 detrital zircons from the sandstone at the top of the Liantuo Formation in the Huangniuyan Section of the Three Gorges area were measured for U-Pb dating and Lu-Hf isotopic compositions. The U-Pb ages of the zircons from the Huangniuyan Section cluster at~800-880 Ma, ~2 000 Ma, ~2 500 Ma, ~2 700 Ma, among which the youngest zircon age is 724±8 Ma. According to the previous geochronological study of tuff on the top of the Liantuo Formation, the sedimentary age of the sandstone in the upper most part of the Liantuo Formation is limited to~724-714 Ma. The sedimentary time of the Liantuo sandstone is close to the U-Pb age of the youngest detrital zircon, which may reflect a rapid recycling of crustal materials. The Hf isotopic two-stage model ages (T_DM2) of zircon are concentrated at~3.7-3.1 Ga, ~2.5-2.0 Ga and~1.3-1.0 Ga, which indicates that the provenance of the sandstone has juvenile crustal growth in the Paleo-Mesoarchean, Paleoproterozoic and Late Mesoproterozoic. By comparing the detrital zircon U-Pb ages and Hf isotopic data from different sections of the Liantuo Formation in the nucleus of the Yangtze craton reported in recent years, it is suggested that the Huangniuyan Section has distinct detrital zircon U-Pb ages and Hf isotopic compositions compared with the Wangfenggang Section, revealing different provenance between them.
- Yangtze block,
- Liantuo Formation,
- detrital zircon,
- U-Pb age,
- Hf isotope,
- petrology

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References(60)

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Detrital Zircon Compositions of U-Pb Ages and Hf Isotope for Sandstone of Liantuo Formation from Three Gorges Area, Yangtze Block and Its Geological Significance

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