华北板块中部晚二叠世-早三叠世砂岩碎屑锆石U-Pb定年及物源判别

冯志强; 刘永江; 王权; 史建儒; 魏荣珠; 卫彦升; 雷勇

doi:10.3799/dqkx.2022.071

Volume 48 Issue 4

Apr. 2023

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Article Navigation > Earth Science > 2023 > 48(4): 1288-1306

Feng Zhiqiang, Liu Yongjiang, Wang Quan, Shi Jianru, Wei Rongzhu, Wei Yansheng, Lei Yong, 2023. Detrial Zircon U-Pb Dating and Provenance Analysis for Late Permian-Early Triassic Sandstone in Central North China Craton. Earth Science, 48(4): 1288-1306. doi: 10.3799/dqkx.2022.071

Citation:

Feng Zhiqiang, Liu Yongjiang, Wang Quan, Shi Jianru, Wei Rongzhu, Wei Yansheng, Lei Yong, 2023. Detrial Zircon U-Pb Dating and Provenance Analysis for Late Permian-Early Triassic Sandstone in Central North China Craton. Earth Science, 48(4): 1288-1306. doi: 10.3799/dqkx.2022.071

Citation:

Feng Zhiqiang, Liu Yongjiang, Wang Quan, Shi Jianru, Wei Rongzhu, Wei Yansheng, Lei Yong, 2023. Detrial Zircon U-Pb Dating and Provenance Analysis for Late Permian-Early Triassic Sandstone in Central North China Craton. Earth Science, 48(4): 1288-1306. doi: 10.3799/dqkx.2022.071

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Detrial Zircon U-Pb Dating and Provenance Analysis for Late Permian-Early Triassic Sandstone in Central North China Craton

doi: 10.3799/dqkx.2022.071

1.
Department of Earth Science and Engineering, Taiyuan University of Technology, Taiyuan 030024, China
2.
Shanxi Institute of Geological Survey, Taiyuan 030006, China
3.
Key Laboratory of Submarine Geosciences and Prospecting Techniques of Ministry of Education, Institute for Advanced Ocean Study, College of Marine Geosciences, Ocean University of China, Qingdao 266100, China
4.
Laboratory for Marine Mineral Resources, Qingdao National Laboratory for Marine Science and Technology, Qingdao 266237, China
5.
Shanxi Museum of Geology, Taiyuan 030021, China
6.
College of Resource and Environment, Shanxi Agricultural University, Jinzhong 030801, China

Received Date: 2021-12-27
Publish Date: 2023-04-25

Abstract

Abstract

The Permian-Triassic stratum of North China craton is well known for its extensive distribution, special lithology, marine-terrestrial transition system and significant division of sedimentary lithology. The predecessors have discussed sedimentary age and source of the Permian-Triassic sandstones, but there is still much controversy. In this study, five sandstone samples are selected from the eastern Ordos basin (Liulin area, Liujiagou and Sunjiagou formations) and Qinshui basin (Qinshui area, Sunjiagou Formation) in Shanxi Province of the central North China craton for LA-ICP-MS U-Pb dating of detrital zircons and geochemical analysis, with the attempt to determine the maximum sedimentary age and its provenance. The geochronology results show that detrital zircons (n=364) from five samples are composed mainly of the Paleozoic and Precambrian magmatic zircons. Among them, the Paleozoic zircons account for 21% with peak ages of ~275 Ma (218-333 Ma; n=65) and ~431 Ma (368-442 Ma; n=10), while the Precambrian zircons account for 79% with distinct peak ages of ~1 888 Ma (1 562-2 222 Ma; n=178) and ~2 529 Ma (2 253-3 167 Ma; n=111). By using the youngest single detrital zircons ages (YSG) and TuffZirc (Zircon Age Extractor)(+6), it obtained different maximum sedimentary ages of 253±7 Ma and 250±7 Ma for the Liujiagou Formation, as well as 256±7 Ma (MSWD=1.1, n=31), 264±11 Ma (MSWD=4.3, n=7), and 250±6 Ma (MSWD=3.6, n=6) for the Sunjiagou Formation, respectively, which is close to the Permian/Triassic boundary age 251.0±0.4 Ma. Based on these results, it constrains that the Liujiagou Formation formed in the Early Triassic and Sunjiagou Formation formed in the Late Permian, and further presume that the sedimentary timing of northern part of Sunjiagou Formation in Shanxi Province is older than southern part. The main material sources of the Permian-Triassic sandstones (Liujiagou and Sunjiagou Formations) are from the Late Paleozoic intrusive rocks in the Inner Mongolia uplift at the northern part of North China craton and the metamorphic basement of North China craton, while a few material sources are from granitic intrusive rocks in southern Xing-Meng orogenic belt.
- central North China,
- Shanxi Province,
- Late Permian-Early Triassic,
- detrital zircon U-Pb dating,
- provenance analysis,
- structural geology

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