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LI Shengxi, HE Bi, YANG Bo, WEI Zhifu, TAO Gang, GAN Baoping, ZHAO Fei, SUN Pingyuan, ZHAO Zhenguan, HUANG Pengfei. Zircon U-Pb geochronology and geochemistry of the Tagelake monzogranites in South Tianshan block: Constraints on crustal magmatic origin and tectonic setting[J]. GEOLOGY IN CHINA, 2023, 50(2): 622-639. DOI: 10.12029/gc20190320001
Citation: LI Shengxi, HE Bi, YANG Bo, WEI Zhifu, TAO Gang, GAN Baoping, ZHAO Fei, SUN Pingyuan, ZHAO Zhenguan, HUANG Pengfei. Zircon U-Pb geochronology and geochemistry of the Tagelake monzogranites in South Tianshan block: Constraints on crustal magmatic origin and tectonic setting[J]. GEOLOGY IN CHINA, 2023, 50(2): 622-639. DOI: 10.12029/gc20190320001
shu

Zircon U-Pb geochronology and geochemistry of the Tagelake monzogranites in South Tianshan block: Constraints on crustal magmatic origin and tectonic setting

  • 1.

    The Second Institute of Geology and Minerals Exploration Team, Gansu Provincial Bureau of Geology and Minerals Exploration and Development, Lanzhou 730020, Gansu, China

  • 2.

    Xi'an Center, China Geological Survey, Xi'an 710054, Shaanxi, China

  • 3.

    Lanzhou Center for Oil and Gas Resources, Institute of Geology and Geophysics, Chinese Academy of Sciences, Lanzhou 730000, Gansu, China

  • 4.

    School of Environment and Resource, Southwest University of Science and Technology, Mianyang 621010, Sichuan, China

  • 5.

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

Funds: 

the project of China Geological Survey 12120115021701

More Information
  • Author Bio:

    LI Shengxi, male, born in 1986, master, senior engineer, engaged in petrology, geochemistry and regional deposit geology research; E-mail: lishengxidzx@126.com

  • Received Date: March 19, 2019
  • Revised Date: October 26, 2019
  • Available Online: September 25, 2023
    Graphical Abstract
    • Abstract

  • This paper is the result of geological survey engineering.

    Objective 

    The Tagelake strip pluton, outcropped at the south Tianshan terrane in Southwestern Tianshan orogenic belt, is composed of monzogranites. Determining the formation mechanism of the monzogranites has important implications for the crust-derived magma origin and the time limit of subduction and ocean basin closure in South Tianshan Mountains.

    Methods 

    In order to determine the formation mechanism of the monzogranites, detailed zircon U-Pb geochronology, major elements and trace elements were firstly conducted.

    Results 

    LA-ICP-MS zircon geochronology study reveals that the monzogranites in the Tagelake area crystallized at (284.0±1.9)-(284.3±3.2) Ma, indicative of an Early Permian pluton. The results of major elements and trace elements reveal that the monzogranites display the characteristics of A-type granite: (1) The contents of SiO2 (70.92%-72.78%), K2O+Na2O (7.91%-8.44%) and A/CNK (0.89-0.99) are high, indicating that monzogranites are metaluminous rock and belongs to the high potassium calcium alkaline series; (2) The monzogranites are enriched in LREE (196×10-6-280×10-6) and depleted in HREE (22.8×10-6-28.2×10-6). Negative Eu anomaly is obvious, with δEu values of 0.51-0.64, and the monzogranites are characterized by fractionated chondrite-normalized REE patterns; (3) The monzogranites are enriched in Rb, Th, K and other large ion lithophile elements and depleted in Nb, Ta, Zr, P, and other high field strength elements.

    Conclusions 

    Combined with the regional tectonic evolution, it is considered that the Tagelake monzogranites were formed in the post-collision tectonic setting.

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