Provenance evolution of the Late Cretaceous uranium–bearing sediments in the southern Daqing placanticline of the northern Songliao Basin: Evidence from detrial zircon U–Pb chronology

LIU Huajian; JIN Ruoshi; XU Zenglian; TANG Chao; DUAN Ming; XIAO Peng; WEI Jialin; ZHANG Pengpeng

doi:10.12029/gc20210427001

2025 Vol. 52, No. 3

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Article navigation > Geology in China > 2025 > 52(3): 1036-1054

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LIU Huajian, JIN Ruoshi, XU Zenglian, TANG Chao, DUAN Ming, XIAO Peng, WEI Jialin, ZHANG Pengpeng. 2025. Provenance evolution of the Late Cretaceous uranium–bearing sediments in the southern Daqing placanticline of the northern Songliao Basin: Evidence from detrial zircon U–Pb chronology[J]. Geology in China, 52(3): 1036-1054. doi: 10.12029/gc20210427001

Citation:

LIU Huajian, JIN Ruoshi, XU Zenglian, TANG Chao, DUAN Ming, XIAO Peng, WEI Jialin, ZHANG Pengpeng. 2025. Provenance evolution of the Late Cretaceous uranium–bearing sediments in the southern Daqing placanticline of the northern Songliao Basin: Evidence from detrial zircon U–Pb chronology[J]. Geology in China, 52(3): 1036-1054. doi: 10.12029/gc20210427001

Provenance evolution of the Late Cretaceous uranium–bearing sediments in the southern Daqing placanticline of the northern Songliao Basin: Evidence from detrial zircon U–Pb chronology

1.
Tianjin Centre (North China Geological Science and Technology Innovation Center), China Geological Survey, Tianjin 300170, China
2.
Key Laboratory of Uranium Geology of China Geological Survey, Tianjin 300170, China
3.
Institute of Geophysical and Geochemical Exploration, Chinese Academy of Geological Sciences, Langfang 065000, Hebei, China

Fund Project: Supported by the projects of National Science Foundation of China (No.92162212), National Key Research and Development Program (No.2018YFC0604200), International Geoscience Program (No.IGCP–675) and China Geological Survey (No.DD20190121).

More Information

Author Bio: LIU Huajian, male, born in 1993, engineer, mainly engaged in the sandstone−type uranium deposits geological survey and sedimentary geology research; E-mail: liuhj_geo@163.com

Received Date: 27 April 2021

Revised Date: 22 February 2022

Publish Date: 25 May 2025

Abstract

Abstract

This paper is the result of geological survey engineering.
Objective
The 5th member of Nenjiang Formation, along with Sifangtai Formation and Mingshui Formation at the southern Daqing placanticline of the northern Songliao Basin, has been identified in recent years as important uranium–bearing stratigraphic units. However, the absence of comprehensive studies on provenance evolution has severely hindered further understanding of both palaeogeographic conditions and uranium mineralization mechanisms in this region.
Methods
In this study, we conducted LA–ICP–MS dating of detrital zircons and compared the results with the ages of surrounding rock masses collected around the basin. Integrated the sandstone composition and heavy minerals characteristics, we comprehensively analyzed the provenance evolution from the 5th member of Nenjiang Formation to Mingshui Formation.
Results
The detrital zircon ages exhibit age ranges across the formations: (1) The 5th member of Nenjiang Formation displays three predominant age ranges: 2994−1765 Ma, 281−281 Ma, and 125−79 Ma. (2) Sifangtai Formation exhibits four characteristic age ranges: 2797−1739 Ma, 462−455 Ma, 296−174 Ma, and 125−79 Ma. (3) Mingshui Formation shows three distinct age ranges: 2448−1792 Ma, 237−220 Ma, and 117−87 Ma.
Conclusions
The provenance of the 5th member of Nenjiang Formation was primarily derived from the Zhangguangcai Range, along with the Jihei area to the east and the Liaoyuan area to the southeast of the Songliao Basin. Additionally, the eastern Lesser Xing’an Mountains to the northern Songliao Basin began contributing sediments to Sifangtai Formation. The provenance of Mingshui Formation was mainly sourced from the Zhangguangcai Range and the eastern Lesser Xing’an Mountains. The findings provide important insights for reconstructing Late Cretaceous paleogeography and understanding the tectonic evolution of Daqing placanticline.
- sandstone–type uranium deposits /
- sedimentary basin /
- provenance analysis /
- detrital zircon U–Pb dating /
- 5th member of Nenjiang Formation /
- Sifangtai Formation /
- Mingshui Formation /
- geological survey engineering /
- southern Daqing placanticline

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References

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