Volume 44 Issue 10
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Zhang Jingbo, An Fang, Wei Shaoni, 2019. Geochronology and Geochemistry of Granite in Tulasu Pluton in West Tianshan, and Its Geological Significance. Earth Science, 44(10): 3495-3511. doi: 10.3799/dqkx.2018.320
Citation: Zhang Jingbo, An Fang, Wei Shaoni, 2019. Geochronology and Geochemistry of Granite in Tulasu Pluton in West Tianshan, and Its Geological Significance. Earth Science, 44(10): 3495-3511. doi: 10.3799/dqkx.2018.320
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Geochronology and Geochemistry of Granite in Tulasu Pluton in West Tianshan, and Its Geological Significance

doi: 10.3799/dqkx.2018.320
  • 1.

    State Key Laboratory of Continental Dynamics, Department of Geology, Northwest University, Xi'an 710069, China

  • 2.

    College of Geology and Environment, Xi'an University of Science and Technology, Xi'an 710054, China

  • Received Date: 2018-12-17
  • Publish Date: 2019-11-11
    Abstract
  • Tulasu pluton in Chinese West Tianshan is located in the northeastern of Tulasu basin, composed of three lithofacies, i. e. quartzdiorite, pyroxene diorite and granite. The granites are composed of granodiorite porphyrite and granite porphyry, characterized by high silicon, high aluminum, enrichment of alkali, Rittman index(σ)=1.61-3.18, A/CNK=1.00-1.09, A/NK=1.07-1.68, belonging to metaluminous-weakly peraluminous high-K calc-alkaline granite. They are relatively enriched in LILEs (Rb, Th, U), extremely poor in Nb, Ta, Sr, P, Ti, etc., obviously fractionated in LREE and HREE, (La/Yb)N=7.48-12.12, showing a medium negative Eu anomaly and no Ce anomaly, δEu=0.47-0.62. But granite porphyry has higher alkali content, more close to shoshonite series and Sr, P, Ti strongly negative, indicating increased involvement of crustal materials. Zircon LA-ICP-MS U-Pb dating for the granite yields an age of 305.9±5.9 Ma. Analyses on zircon Hf isotopic compositions yield positive εHf(t) values varying from +0.4 to +8.7, implying that the involvement of mantle-derived magmatic materials during the formation of granite; TDM2 varies from 766 to 1 294 Ma, showing that magma was derived from Proterozoic-Neoproterozoic crust. By comparison, it is concluded that fractional crystallization enhanced, involvement of crustal materials increased from granodiorite to granite porphyry. The granite was formed in post-collisional setting.

     

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