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Volume 35 Issue 4
Aug 2024
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Zuochen Li, Xianzhi Pei, Liyong Wei, Guobing Liang, Meng Wang, Ruibao Li, Lei Pei, Chengjun Liu, Youxin Chen, Feng Gao. Detrital Zircon Geochronology of Early Triassic Strata in the West Qinling Orogen: Implications for the Tectonic Evolution of the Paleo-Tethyan Ocean. Journal of Earth Science, 2024, 35(4): 1087-1106. doi: 10.1007/s12583-022-1714-1
Citation: Zuochen Li, Xianzhi Pei, Liyong Wei, Guobing Liang, Meng Wang, Ruibao Li, Lei Pei, Chengjun Liu, Youxin Chen, Feng Gao. Detrital Zircon Geochronology of Early Triassic Strata in the West Qinling Orogen: Implications for the Tectonic Evolution of the Paleo-Tethyan Ocean. Journal of Earth Science, 2024, 35(4): 1087-1106. doi: 10.1007/s12583-022-1714-1

Detrital Zircon Geochronology of Early Triassic Strata in the West Qinling Orogen: Implications for the Tectonic Evolution of the Paleo-Tethyan Ocean

doi: 10.1007/s12583-022-1714-1
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  • Corresponding author: Xianzhi Pei, peixzh@163.com
  • Received Date: 25 May 2022
  • Accepted Date: 27 Jul 2022
  • Available Online: 16 Aug 2024
  • Issue Publish Date: 30 Aug 2024
  • The West Qinling Orogen (WQO) is located in the western part of the Qinling Orogen and in the transition zone of Qilian Orogen, Songpan-Garze Orogen and Yangtze Block, and also the key position of Triassic collision orogenic event. The study of the Early Triassic strata in the WQO is contributed to analyze the closure process of the paleo-Tethys. We conducted LA-ICP-MS U-Pb dating studies on detrital zircons to determine the provenance, depositional age, and tectonic setting of the Early Triassic Longwuhe Formation in the Lintan area of the WQO. The results show that the majority of the detrital zircons in the Longwuhe Formation are mainly magmatic origin and have characteristic of crust source zircon. The lowest limit of sedimentation of the Longwuhe Formation is constrained to the Early Triassic, with the youngest detrital zircon age of 253 ± 3 Ma. The ages can be divided into five age groups: 3 346–1 636 Ma, with two peak ages of ca. 2 495 and ca. 1 885 Ma; 1 585–1 010 Ma, with a peak age at ca. 1 084 Ma; 992–554 Ma, with a peak age at ca. 939 Ma; 521–421 Ma, with a peak age at ca. 445 Ma; 418–253 Ma, with a peak age at ca. 280 Ma. Apparently, the sources of the Longwuhe Formation include the northern margin of the WQO, the Qilian Orogen (QLO) and the basement of the southern margin of the North China Block (NCB), of which the ancient basement of the southern margin of the NCB is the main source area of the Longwuhe Formation. Combined with previous studies, we propose that the Longwuhe Formation was formed in a fore-arc basin, which is related to the closure of the A'nyemaqen-Mianlüe Ocean from the Early Permian to Early–Middle Triassic due to the northward subduction-collision of the Yangtze Block (YZB). This also indicates that the A'nyemaqen-Mianlüe Ocean has flat subduction characteristics.

     

  • Electronic Supplementary Materials: Supplementary materials (Tables S1–S4) are available in the online version of this article at https://doi.org/10.1007/s12583-022-1714-1.
    Conflict of Interest
    The authors declare that they have no conflict of interest.
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