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XU Qiangwei, WANG Pin, WANG Zhiqiang, WANG Chengming, ZHENG Yi, FANG Jing. Zirzon U-Pb age and petrogenisis of plagiogranite porphyry in Changlingzi, Hexigten Banner, Inner Mongolia and its collision orogeny[J]. GEOLOGY IN CHINA, 2021, 48(1): 229-246. DOI: 10.12029/gc20210116
Citation: XU Qiangwei, WANG Pin, WANG Zhiqiang, WANG Chengming, ZHENG Yi, FANG Jing. Zirzon U-Pb age and petrogenisis of plagiogranite porphyry in Changlingzi, Hexigten Banner, Inner Mongolia and its collision orogeny[J]. GEOLOGY IN CHINA, 2021, 48(1): 229-246. DOI: 10.12029/gc20210116
shu

Zirzon U-Pb age and petrogenisis of plagiogranite porphyry in Changlingzi, Hexigten Banner, Inner Mongolia and its collision orogeny

  • 1.

    School of Earth and Space Science, Peking University, Beijing 100871, China

  • 2.

    Key Laboratory of Marginal Sea Geology, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou 510301, Guangdong, China

  • 3.

    School of Resources and Environmental Engineering, Hefei University of Technology, Hefei 230009, Anhui, China

  • 4.

    School of Earth Sciences and Geological Engineering, Sun Yat-sen University, Guangzhou 510275, Guangdong, China

  • 5.

    Institute of Deep-Sea Science and Engineering, Chinese Academy of Sciences, Sanya 572000, Hainan, China

Funds: 

National Natural Science Foundation of China 4160206

the program Jinda Mining Development Co., Ltd., of Hexigten Banner, Inner Mongolia 20150008

More Information
  • Author Bio:

    XU Qiangwei, male, born in 1986, doctor, majors in mineralogy, petrology and metallogeny; E-mail:qwxu@pku.edu.cn

  • Corresponding author:

    WANG Pin, female, born in 1987, doctor, majors in mineralogy, petrology and metallogeny; E-mail:wangpin@scsio.ac.cn

  • Received Date: April 02, 2018
  • Revised Date: August 14, 2018
  • Available Online: September 25, 2023
    Graphical Abstract
    • Abstract

  • The Changlingzi plagiogranite porphyry is located in the Xilinhot Late Paleozoic Accretion Complex within the Da Hinggan Mountains. This study is focused on the zircon U -Pb isotopic geochronology, Hf isotopic composition analysis and geochemistry of the Changlingzi plagiogranite porphyry. Zircon crystals from the plagiogranite porphyry yielded weighted average 206Pb/238U age of (248.1±4.7)Ma. The zircons from this porphyry have positive εHf(t) values from 5.78 to 12.41, with TDM2(Hf) ages from 914 to 488Ma. The plagiogranite porphyry has high content of SiO2, Na2O and Al2O3, and low content of TiO2, MgO and CaO, showing a metaluminous-peraluminouslow-K to calc-alkaline affinity, with LREE enrichment and HREE depletion, suggesting I-type granite. In addition, the plagiogranite porphyry has high Sr and low Y values as well as high Sr/Y ratios (74.5~103.4), indicating that the plagiogranite porphyry belongs to adakite. It is suggested that the plagiogranite porphyry was formed by partial melting of the thickened newborn lower crust. And in Early Triassic, Xing' an-Mongolian orogenic belt was in a collisionorogeny tectonic setting, indicating that the Paleo-Asian Ocean had been closed in this period.

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