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    中国百强科技报刊

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    Volume 37 Issue 3
    May  2012
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    Article Contents
    YANG Wen-tao, YANG Jiang-hai, WANG Xiao-feng, DU Yuan-sheng, 2012. Geochronology from Middle Triassic to Middle Jurassic Detrital Zircons in Jiyuan Basin and Its Implications for the Qinling Orogen. Earth Science, 37(3): 489-500. doi: 10.3799/dqkx.2012.055
    Citation: YANG Wen-tao, YANG Jiang-hai, WANG Xiao-feng, DU Yuan-sheng, 2012. Geochronology from Middle Triassic to Middle Jurassic Detrital Zircons in Jiyuan Basin and Its Implications for the Qinling Orogen. Earth Science, 37(3): 489-500. doi: 10.3799/dqkx.2012.055

    Geochronology from Middle Triassic to Middle Jurassic Detrital Zircons in Jiyuan Basin and Its Implications for the Qinling Orogen

    doi: 10.3799/dqkx.2012.055
    • Received Date: 2011-05-10
      Available Online: 2021-11-09
    • Publish Date: 2012-05-01
    • Jiyuan basin is located in the north of Qinling orogen and regarded as a Triassic-Jurassic synorogenic basin. This paper presents a great number of detrital zircon U-Pb ages for synorogenic sediments in age ranging from the Middle Triassic to Middle Jurassic in the Jiyuan basin. The results show seven major age groups at 2.9-1.7 Ga, 1.6-1.0 Ga, 1.0-0.8 Ga, 800-650 Ma, 520-380 Ma, 350-245 Ma and ~220 Ma. It is obvious that age group of 2.9-1.7 Ga is directly derived from the Precambrian basement of North China Craton whereas other groups are typical characteristics of the Qinling orogenic belt. An important observation is that the Qinling-sourced detrital zircons become older from the Middle Triassic to the Early Jurassic sedimentary sequences, which is characterized by the main age clusters at 350-245 Ma occurring in the T2-T31 strata while age groups at 1.6-1.0 Ga, 1.0-0.8 Ga, 800-650 Ma and 520-380 Ma increase successively in the T32-J21 samples. In addition, little grains of age groups at 1.6-1.0 Ga, 520-380 Ma and ~220 Ma are presented in the J22 sample. The above-mentioned findings indicate that unroofing pattern of Qinling orogenic belt developed by the denudation of sendiments from young covers to old basements in order, then to the Carnian plutons. Integrated with the data reported from Hefei and Huangshi basins, it is well established that the intensity of unroofing increased from the west to the east in the Early Jurassic, and the denudation timing of the ultra high pressure (UHP)-high pressure (HP) rocks or Carnian plutons changed successively from the Early Jurassic in the east to the Middle Jurassic in the west.

       

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