扬子东南缘两界河组碎屑锆石U-Pb年龄及其对Sturtian冰川作用的启示

高永娟; 张予杰; 安显银; 刘石磊; 郑杰; 桑永恒

doi:10.3799/dqkx.2020.153

Volume 45 Issue 8

Aug. 2020

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Article Navigation > Earth Science > 2020 > 45(8): 3070-3081

Gao Yongjuan, Zhang Yujie, An Xianyin, Liu Shilei, Zheng Jie, Sang Yongheng, 2020. Detrital Zircon U-Pb Ages of Liangjiehe Formation in East Guizhou Province and Its Implications for Sturtian Glaciation. Earth Science, 45(8): 3070-3081. doi: 10.3799/dqkx.2020.153

Citation:

Gao Yongjuan, Zhang Yujie, An Xianyin, Liu Shilei, Zheng Jie, Sang Yongheng, 2020. Detrital Zircon U-Pb Ages of Liangjiehe Formation in East Guizhou Province and Its Implications for Sturtian Glaciation. Earth Science, 45(8): 3070-3081. doi: 10.3799/dqkx.2020.153

Citation:

Gao Yongjuan, Zhang Yujie, An Xianyin, Liu Shilei, Zheng Jie, Sang Yongheng, 2020. Detrital Zircon U-Pb Ages of Liangjiehe Formation in East Guizhou Province and Its Implications for Sturtian Glaciation. Earth Science, 45(8): 3070-3081. doi: 10.3799/dqkx.2020.153

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Detrital Zircon U-Pb Ages of Liangjiehe Formation in East Guizhou Province and Its Implications for Sturtian Glaciation

doi: 10.3799/dqkx.2020.153

1.
Chengdu Center of China Geological Survey, Chengdu 610081, China
2.
College of Earth Sciences, Chengdu University of Technology, Chengdu 610059, China

Received Date: 2020-03-23
Publish Date: 2020-08-15

Abstract

Abstract

The Liangjiehe Formation is the interglacial stratum between Chang'an and Gucheng glaciations in the southeastern Yangtze Block, and the lithology is dominated by detrital sandstone and quartz sandstone. For a better understanding of the temporal and spatial distribution of the Sturtian glacigenic strata in South China, it is important to determine the depositional age of the Liangjiehe Formation. In this study, systematical morphology and zircon U-Pb dating were carried out on detrital zircons from the Liangjiehe Formation in the eastern Guizhou. Most of the detrital zircons are of magmatic origin, and have a main ²⁰⁶Pb/²³⁸U age range of 740-900 Ma and minor populations of Paleoproterozoic-Archean ages, with peaks at~760 Ma, ~780 Ma, ~800 Ma, ~820 Ma and 880-900 Ma. The youngest single-grain zircon obtained at the bottom of the Liangjiehe Formation gives the age of 708±15 Ma, and the youngest single-grain zircon from the upper part gives the age of 703±22 Ma. Taking into account the topmost age~690 Ma of the contemporary stratum (Xieshuihe Formation), it is suggested that the Liangjiehe Formation was most likely deposited at 708-690 Ma. The detrital zircon U-Pb age spectrum of the Liangjiehe Formation records the Neoproterozoic episodic tectonic-magmatic events and the information for the early crustal evolution of Yangtze Block. The zircon morphology indicates that the provenances of the Liangjiehe Formation may include the underlying Neoproterozoic magmatic and sedimentary strata, and the basement rocks from the northwestern and southwestern Yangtze Block. The detrital zircon U-Pb dating at the bottom of the Liangjiehe Formation constrained the interglacial deposition later than~708 Ma. Considering that the stratigraphic distribution in the early Nanhua period is partly controlled by basin tectonic activities, the Chang'an glacial deposit may exist locally in eastern Guizhou.
- Yangtze Block,
- Liangjiehe Formation,
- detrital zircon,
- Jiangkou glaciation,
- interglaciation,
- geochronology

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References(49)

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Detrital Zircon U-Pb Ages of Liangjiehe Formation in East Guizhou Province and Its Implications for Sturtian Glaciation

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