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    Volume 44 Issue 4
    Apr.  2019
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    Article Navigation >  Earth Science  > 2019  >  44(4): 1338-1356
    Li Peng, Pei Xianzhi, Li Ruibao, Li Zuochen, Yang Yunjun, Chen Youxin, Liu Chengjun, Wang Meng, Pei Lei, Gao Feng, Su Zhenguo, Liang Guobing, Gao Xiangyu, 2019. Zircon U-Pb Geochronology, Geochemistry and Geological Significance of Daan Granite in Northwestern Margin of Yangtze Block. Earth Science, 44(4): 1338-1356. doi: 10.3799/dqkx.2018.163
    Citation: Li Peng, Pei Xianzhi, Li Ruibao, Li Zuochen, Yang Yunjun, Chen Youxin, Liu Chengjun, Wang Meng, Pei Lei, Gao Feng, Su Zhenguo, Liang Guobing, Gao Xiangyu, 2019. Zircon U-Pb Geochronology, Geochemistry and Geological Significance of Daan Granite in Northwestern Margin of Yangtze Block. Earth Science, 44(4): 1338-1356. doi: 10.3799/dqkx.2018.163
    shu

    Zircon U-Pb Geochronology, Geochemistry and Geological Significance of Daan Granite in Northwestern Margin of Yangtze Block

    doi: 10.3799/dqkx.2018.163
    • 1.

      School of Earth Science and Resources, Chang'an University, Xi'an 710054, China

    • 2.

      Key Laboratory of Western Mineral Resources and Geological Engineering, Ministry of Education, Xi'an 710054, China

    • 3.

      Shaanxi Center of Geological Survey, Xi'an 710065, China

    • Received Date: 2018-05-04
    • Publish Date: 2019-04-15
      Abstract
    • Located in the Ningqiang area of the northwest margin of the Yangtze block, the Daan granite consists mainly of biotite granodiorite. However, the petrogenesis and geological significances of the Daan pluton remain unclear in addition to the controversial formation age. In this paper, a detailed study of LA-ICP-MS zircon U-Pb geochronology and geochemistry is presented for the Daan granite.The results show that the age of granodiorite is 212.3±1.6 Ma and 212.48±0.43 Ma, belonging to the Late Triassic. Geochemically, the Daan granites have relatively high SiO2 (67.61%-69.02%) and Al2O3 (16.14%-16.80%) contents, and are enriched in LILE (Cs, Ba) and LREE. The samples display an insignificant negative Eu anomaly, low Y (3.10×10-6-3.90×10-6) contents, and high Sr contents (538×10-6-907×10-6) and Sr/Y ratios (138-291), exhibiting marked geochemical features of adakite. Combined with regional geological data, it is proposed that the Daan granite was formed in a post-collisional tectonic environment. The extensional regime after collision between the North China block and the Yangtze block induced the upwelling of mantle material, resulting in the dehydration and melting of thickened basic lower crust and formed the adakitic magma.

       

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