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2022 Vol. 49, No. 6
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ZHOU Yu, ZHOU Xiong, ZHANG Yi, QIN Zhipeng, JIA Zhiquan, LIANG Bing. 2022. Geochemistry, zircon geochronology and Lu-Hf isotopic characteristics of the Sudi monzogranite in the Western Sichuan: Implications for tectonic setting of the Songpan-Ganze terrane[J]. Geology in China, 49(6): 1984-2001. doi: 10.12029/gc20220620
Citation: ZHOU Yu, ZHOU Xiong, ZHANG Yi, QIN Zhipeng, JIA Zhiquan, LIANG Bing. 2022. Geochemistry, zircon geochronology and Lu-Hf isotopic characteristics of the Sudi monzogranite in the Western Sichuan: Implications for tectonic setting of the Songpan-Ganze terrane[J]. Geology in China, 49(6): 1984-2001. doi: 10.12029/gc20220620
shu

Geochemistry, zircon geochronology and Lu-Hf isotopic characteristics of the Sudi monzogranite in the Western Sichuan: Implications for tectonic setting of the Songpan-Ganze terrane

  • 1.

    Urumqi Natural Resources Comprehensive Survey Center of China Geological Survey, Urumqi 830057, Xinjiang, China

  • 2.

    Institute of Multipurpose Utilization of Mineral Resources, Chinese Academy of Geological Sciences, Chengdu 610041, Sichuan, China

  • 3.

    Chengdu University of Technology, Chengdu 610059, Sichuan, China

  • 4.

    No. 108 Geological Team, BGEEMRSP, Chongzhou 611230, Sichuan, China

    • Fund Project: Supported by the projects of China Geological Survey (No.DD20160074, DD20190185, DD20211550 and ZD20220316), National Natural Science Foundation of China (No.41602072), Science and Technology Department of Tibet(No. XZ201801-GB-01), Natural Science Foundation of Xinjiang Uygur Autonomous Region(No.2022D01A148)
More Information
  • Author Bio: ZHOU Yu, born in 1984, doctor, majors in the research of magmatic rock and its mineralization; E-mail: zhouyu46@163.com
Received Date:  21 February 2019
Revised Date:  20 April 2020
Publish Date:  25 December 2022
    Abstract

  • This paper is the result of geological survey engineering.

     Objective

    It is of great significance to find out the geochemical and tectonic evolution characteristics of granite in the southeast of the Songpan-Ganze terrane for searching for rare metal minerals in this area.

     Methods

    we have carried out field geological survey and conducted whole-rock geochemistry and zircons LA-(MC)-ICP-MS U-Pb and Lu-Hf isotope analyses on the monzogranite of the Sudi pluton in the southeast part of the Songpan-Ganze terrane.

     Results

    The results show that the samples were medium-high potassium, sodium rich and calcium deficiency. The values of AR were 1.44-1.83 and values of A/CNK were 0.98-1.16, which were medium-high potassium calcareous alkaline series. The rocks show relatively enriched large ion lithophile element (LILE), negative high field-strength elements (HFSE), and high REE content (the total amount of REE = 157.16×10-6-187.88×10-6) with the LREE enrichement (LREE/HREE = 6.26-9.46) and weak negative Eu anomaly europium anomaly (δEu = 0.62-0.74). The results of zircon U-Pb dating were (221.1±1.5) Ma (MSWD=0.30, n=22) and (214.5±1.5) Ma (MSWD=0.22, n=22), indicating that the primitive magma of the Sudi pluton crystallized in the middle of the Late Triassic. Its zircon Lu-Hf isotope εHf(t) and TDM2 are -6.56--4.12 and 1.67-1.51 Ga.

     Conclusions

    According to the comprehensive analysis, we believe that the monzogranite in Sudi pluton is a typical I-type granite and it may be formed by the upwelling and emplacement of the initial magma from the lower crust in the middle of Late Triassic in the process of orogenic collision to post-collisional extensional tectonic setting. The southeastern margin of Songpan-Ganze terrane was under post-collisional orogenic environment in Late Triassic.
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