塔里木盆地塔中志留系柯坪塔格组物源示踪：碎屑锆石U-Pb年代学证据

李祥权; 丁洪坤; 彭鹏; 吴梅莲; 钟楚红; 柴雄; 刘国威; 彭丽

doi:10.3799/dqkx.2020.197

Volume 46 Issue 8

Aug. 2021

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Article Navigation > Earth Science > 2021 > 46(8): 2819-2831

Li Xiangquan, Ding Hongkun, Peng Peng, Wu Meilian, Zhong Chuhong, Chai Xiong, Liu Guowei, Peng Li, 2021. Provenance of Silurian Kepingtage Formation in Tazhong Area, Tarim Basin: Evidence from Detrital Zircon U-Pb Geochronology. Earth Science, 46(8): 2819-2831. doi: 10.3799/dqkx.2020.197

Citation:

Li Xiangquan, Ding Hongkun, Peng Peng, Wu Meilian, Zhong Chuhong, Chai Xiong, Liu Guowei, Peng Li, 2021. Provenance of Silurian Kepingtage Formation in Tazhong Area, Tarim Basin: Evidence from Detrital Zircon U-Pb Geochronology. Earth Science, 46(8): 2819-2831. doi: 10.3799/dqkx.2020.197

Citation:

Li Xiangquan, Ding Hongkun, Peng Peng, Wu Meilian, Zhong Chuhong, Chai Xiong, Liu Guowei, Peng Li, 2021. Provenance of Silurian Kepingtage Formation in Tazhong Area, Tarim Basin: Evidence from Detrital Zircon U-Pb Geochronology. Earth Science, 46(8): 2819-2831. doi: 10.3799/dqkx.2020.197

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Provenance of Silurian Kepingtage Formation in Tazhong Area, Tarim Basin: Evidence from Detrital Zircon U-Pb Geochronology

doi: 10.3799/dqkx.2020.197

1.
Hubei Key Laboratory of Marine Geological Resources, China University of Geosciences, Wuhan 430074, China
2.
Key Laboratory of Tectonics and Petroleum Resources of Ministry of Education, China University of Geosciences, Wuhan 430074, China
3.
PetroChina Tarim Oilfield Company, Kuerle 841000, China

Received Date: 2020-03-14
Available Online: 2021-09-14
Publish Date: 2021-08-15

Abstract

Abstract

There is still uncertainty in the understanding of the source of the Silurian sedimentation in Tazhong area of Tarim Basin. Using LA-ICP-MS analysis technology,two samples of the Kepingtage Formation in Tazhong area were collected for detrital zircon U-Pb chronology. The results show that the zircons are mainly of magmatic crystallization origin and their ages are mainly distributed in four periods: Early Paleozoic 460-490 Ma,Neoproterozoic 760-1 000 Ma,Paleoproterozoic 1 600-2 200 Ma,and Late Neoarchaean-Early Paleoproterozoic 2 400-2 600 Ma. The Neoproterozoic 760-1 000 Ma detrital zircon ages take the largest proportion (56.8%),with a~850 Ma single peak. Based on the plate dynamics background of the northern and southern margins of the Tarim plate during the Silurian Period,the analysis of tectonic evolution and geomorphologic features within the basin,as well as the detailed comparison of zircon ages with the potential provenance area,it is proposed that the Tazhong Silurian detrital zircons were mainly sourced from the Tiekelike uplift in the southwest margin of Tarim Basin.
- provenance,
- detrital zircon,
- U-Pb chronology,
- Kepingtage Formation,
- Silurian,
- Tazhong area,
- Tarim Basin

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References(113)

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Provenance of Silurian Kepingtage Formation in Tazhong Area, Tarim Basin: Evidence from Detrital Zircon U-Pb Geochronology

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