Detrital zircon U-Pb ages of Middle-Late Permian sedimentary rocks from the southwestern margin of the North China Craton: Implications for provenance and tectonic evolution

The southwestern margin of the North China Craton (NCC) is located between the Alxa Terrane to the northwest, the North Qilian Orogen to the west and the North Qinling Orogen to the south. However, the paleogeographic and tectonic evolution for the southwestern part of the NCC in the Late Paleozoic is still poorly constrained. In order to constrain the Late Paleozoic tectonic evolution of the southwestern NCC, we carried out detailed field work and detrital zircon U-Pb geochronological research on Middle-Late Permian sedimentary rocks at the southwestern margin of the NCC. The U-Pb age spectra of detrital zircons from six samples are similar, showing four populations of 2.6-2.4 Ga, 2.0-1.7 Ga, 500-360Ma and 350-250Ma. Moreover, on the basis of the weighted-mean age of the youngest detrital zircons (257 +/- 4Ma), combined with the published results and volcanic interlayers, we propose that the Shangshihezi Formation formed during the Middle-Late Permian. Our results and published data indicate that the detrital zircons with age groups of 2.6-2.4 Ga and 2.0-1.7 Gawere likely derived from the Khondalite Belt and Yinshan Block in the northwestern NCC. The junction part between the North Qinling and North Qilian Orogen may provide the 500-360 Ma detrital zircons for the study area. The 350-250 Ma detrital zircons were probably derived fromthe northwestern part of the NCC. The majority of materials from Shangshihezi Formation within the study area were derived from the northwestern part of the NCC, indicating that the northwestern part of the NCC was strongly uplifted possibly resulting from the progressive subduction and closure of the Paleo-Asian Ocean. A small amount of materials were sourced from southwestern part of the NCC, indicating that the North Qinling Orogen experienced a minor uplift resulting from the northward subduction of the South Qinling terrane. (C) 2020 International Association for Gondwana Research. Published by Elsevier B.V. All rights reserved.