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| Citation: | Wang Yilong, Zhou Wanpeng, Liu Pinghua, Tian Zhonghua, Zhang Yujia, 2022. Depositional Timing and Provenance Characteristics of the Early Paleozoic Gaotan Formation in the Wugongshan Area, Jiangxi Province: New Evidence from Detrital Zircon U-Pb Dating and Rare Earth Element Compositions of Garnet-Bearing Mica Quartz Schist. Earth Science, 47(3): 1078-1093. doi: 10.3799/dqkx.2022.005
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The Gaotan Formation, which has undergone greenschist to amphibolite facies metamorphism, is one of the most widely distributed Early Paleozoic strata units in the Wugongshan complex of Jiangxi Province. Depositional timing and provenance of the Gaotan Formation is vital for probing the Early Paleozoic crustal evolutionary of the Wugongshan complex. In this paper, LA-ICP-MS (laser ablation inductively coupled plasma mass spectrometry) was used to analyze the zircon U-Pb ages and rare earth element compositions of bearing-garnet micas quartz schist in the Gaotan Formation of the Wugongshan complex. The age of the youngest group of detrital zircons from the garnet-bearing micas quartz schist is 524±12 Ma, combined with geological relationship which the Gaotan Formation was intruded by the ca. 462 Ma granites in the Wugongshan complex, it is speculated that the depositional timing of the Gaotan formation is 524-462 Ma. Detrital zircon U-Pb ages of the Gaotan Formation range from 3 622 Ma to 497 Ma, with the main age peak of 956 Ma and four secondary age peaks of 2 456 Ma, 1 644 Ma, 850 Ma and 524 Ma, respectively. By comparing the detrital zircon ages of the Early Paleozoic sedimentary rocks in the Yangtze and Cathaysia blocks, the provenance characteristics of the Gaotan Formation are similar to the Early Paleozoic strata in the Cathaysia block, indicating that the Wugongshan complex was a part of the Cathaysia block during the Early Paleozoic.
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dqkxzx-47-3-1078-附表.docx
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