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    Volume 44 Issue 7
    Jul.  2019
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    Article Navigation >  Earth Science  > 2019  >  44(7): 2353-2367
    Gao Zhongwei, Xie Chaoming, Ren Yunsheng, Liu Jinheng, Li Linhan, Hao Yujie, 2019. Geochemical Characteristics and LA-ICP-MS Zircon U-Pb Age of the Azhalang Intrusion in Sumdo, Southern Tibet. Earth Science, 44(7): 2353-2367. doi: 10.3799/dqkx.2018.945
    Citation: Gao Zhongwei, Xie Chaoming, Ren Yunsheng, Liu Jinheng, Li Linhan, Hao Yujie, 2019. Geochemical Characteristics and LA-ICP-MS Zircon U-Pb Age of the Azhalang Intrusion in Sumdo, Southern Tibet. Earth Science, 44(7): 2353-2367. doi: 10.3799/dqkx.2018.945
    shu

    Geochemical Characteristics and LA-ICP-MS Zircon U-Pb Age of the Azhalang Intrusion in Sumdo, Southern Tibet

    doi: 10.3799/dqkx.2018.945
    • 1.

      College of Earth Sciences, Jilin University, Changchun 130061, China

    • 2.

      Key Laboratory of Mineral Resources Evaluation in Northeast Asia, Ministry of Natural Resources, Changchun 130061, China

    • Received Date: 2018-11-13
    • Publish Date: 2019-07-15
      Abstract
    • The Azhalang pluton is located in the Sumdo area in the east-central part of the Gangdise magmatic arc. Zircon U-Pb dating and geochemical analysis of the whole rock indicate that the Azhalang intrusion is quartz monzonite porphyry and the formation period is Miocene (17.9±0.2 Ma). Geochemical characteristics show high Sr (1 052×10-6-1 150×10-6), low Y (8.51×10-6-9.04×10-6) and Yb (0.85×10-6-0.94×10-6), high Sr/Y (118-128) and La/Yb (30.9-40.8) ratios, no obvious Eu anomalies, high K2O (3.17%-3.84%) content, low Cr (6.46×10-6-7.78×10-6) and Ni (5.41×10-6-7.45×10-6) content, high Mg# value (43.8-49.8), high Rb/Sr ratio, large ion lithophile element content, such as Rb, Rb, Rb. Ba, Th and U were significantly higher than LREE.These geochemical characteristics indicate that the petrogenesis of the rocks may be formed by partial melting of the thicker lower crust and formed in the post-collisional tectonic setting of the India-Eurasia collision orogeny, and some mantle-derived materials may be involved.This study provides important constraints for revealing the genesis and metallogenic geological setting of the Miocene adakite in the Gangdise metallogenic belt.

       

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