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GAO Feng, JIAN Kunkun, LI Ning, et al. U-Zircon U-Pb Dating and Geochemistry of Jijiquan Pluton in the Eastern Section of Beishan Orogenic Belt and their Tectonic Implications[J]. Northwestern Geology, 2018, 51(3): 26-37.
Citation: GAO Feng, JIAN Kunkun, LI Ning, et al. U-Zircon U-Pb Dating and Geochemistry of Jijiquan Pluton in the Eastern Section of Beishan Orogenic Belt and their Tectonic Implications[J]. Northwestern Geology, 2018, 51(3): 26-37.
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U-Zircon U-Pb Dating and Geochemistry of Jijiquan Pluton in the Eastern Section of Beishan Orogenic Belt and their Tectonic Implications

  • 1. Shaanxi Geological Survey Center, Xi'an 710068, Shaanxi, China;

  • 2. Chang'an University, Xi'an 710054, Shaanxi, China

More Information
  • Received Date: November 06, 2017
  • Revised Date: March 22, 2018
  • Available Online: July 28, 2022
  • Published Date: September 04, 2018
    Graphical Abstract
    • Abstract
  • The Jijiquan plution in the eastern section of Beishan Orogenic Belt consists of gabbro and diabase. The zircon LA-ICP-MS dating has obtained an age of (274.1±5.3) Ma, which reveals that this pluton was formed in Early Permian. The geochemical data shows that these rocks have low SiO2 content, relatively high Al2O3 and CaO content as well as Mg# value, low total REE contents, no obvious fraction of LREE and HREE, weak positive Eu anomly, enrichment of LILE and depletion of HFSE. The geochemical features indicate that the magma was formed by the partial melting of depleted mantle, which was suffered the crust contamination in the magma rising process. After analyzing the regional geological background, it is considered that the Jijiquan pluton was formed at an intraplate extensional tectonic setting.
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