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    Volume 43 Issue 9
    Sep.  2018
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    Article Navigation >  Earth Science  > 2018  >  43(9): 3001-3017
    Sun Zhiyuan, Long Lingli, Wang Yuwang, Luo Zhaohua, Zhao Lutong, Wu Chenghe, 2018. SHRIMP Zircon U-Pb Geochronology and Geochemistry of Diorite Porphyrite in Tongyuliang Copper Deposit, Eastern Tianshan and Its Geological Significance. Earth Science, 43(9): 3001-3017. doi: 10.3799/dqkx.2018.997
    Citation: Sun Zhiyuan, Long Lingli, Wang Yuwang, Luo Zhaohua, Zhao Lutong, Wu Chenghe, 2018. SHRIMP Zircon U-Pb Geochronology and Geochemistry of Diorite Porphyrite in Tongyuliang Copper Deposit, Eastern Tianshan and Its Geological Significance. Earth Science, 43(9): 3001-3017. doi: 10.3799/dqkx.2018.997
    shu

    SHRIMP Zircon U-Pb Geochronology and Geochemistry of Diorite Porphyrite in Tongyuliang Copper Deposit, Eastern Tianshan and Its Geological Significance

    doi: 10.3799/dqkx.2018.997
    • 1.

      School of the Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China

    • 2.

      Beijing Institute of Geology for Mineral Resources, Beijing 100012, China

    • 3.

      Faculty of Land Resource Engineering, Kunming University of Science and Technology, Kunming 650093, China

    • 4.

      Turpan Mining and Matallurgy Co., Ltd., Turpan 838000, China

    • Received Date: 2018-03-20
    • Publish Date: 2018-09-15
      Abstract
    • The Tongyuliang is a newly discovered copper deposit in recent years, which is located in the Aqishan-Yamansu Carboniferous volcanic belt of eastern Tianshan, Xinjiang, NW China. However, the research for this hydrothermal copper deposit is limited. The SHRIMP zircon U-Pb dating of diorite porphyrite which is genetically related with the copper deposit is 317.7±2.4 Ma. It can be inferred that the ore-forming epoch of this deposit may be Late Carboniferous. The major elements data show that the diorite porphyrites contain 56.71%-66.03% of SiO2, 49.75-55.29 of Mg#, 5.15%-6.40% of Na2O+K2O and 4.49-53.62 of Na2O/K2O, and the aluminium index (A/CNK)=0.9-1.1. The diorite porphyrites are relatively enriched in sodium and alumina and belong to the low K (IAT) series. They have low ∑REE (39.56×10-6-60.60×10-6) and are enriched in LREE relative to HREE. The primitive mantle normalized trace elements spider diagram is characterized by Ba, U, K, Sr (large ion lithophile elements) enrichment and Nb, Ta, Ti (high field strength elements) depletion, which shows the island-arc volcanic characteristics. The (87Sr/86Sr)i ratios range from 0.704 030 to 0.704 413, and εNd(t) values vary from 1.02 to 6.42, which indicates that the magma source of diorite porphyrites may be derived from depleted mantle source. The geochronology, geochemistry, and isotope characteristics of diorite porphyrites suggest that the Tongyuliang copper deposit was formed in the arc setting. Combining existing geological data, the ore-bearing materials probably came from the mantle wedge, which had undergone metasomatism induced by southward subduction of Paleo-Kangguer oceanic plate. In early Late Carboniferous, the fluids which contained copper element intruded, and the Tongyuliang copper deposit formed after sub-volcanics replaced their own bodies or volcanic rocks when they reached the upper area.

       

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