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SUN Zhiyuan, LONG Lingli, WANG Yuwang, LUO Zhaohua, ZHAO Lutong, XIE Hongjing. Geochronology, geochemistry and genesis of Na-rich volcanic rocks of the Zhaibeishan copper deposit in Eastern Tianshan Mountains[J]. GEOLOGY IN CHINA, 2018, 45(5): 943-962. DOI: 10.12029/gc20180505
Citation: SUN Zhiyuan, LONG Lingli, WANG Yuwang, LUO Zhaohua, ZHAO Lutong, XIE Hongjing. Geochronology, geochemistry and genesis of Na-rich volcanic rocks of the Zhaibeishan copper deposit in Eastern Tianshan Mountains[J]. GEOLOGY IN CHINA, 2018, 45(5): 943-962. DOI: 10.12029/gc20180505
shu

Geochronology, geochemistry and genesis of Na-rich volcanic rocks of the Zhaibeishan copper deposit in Eastern Tianshan Mountains

  • 1.

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

  • 2.

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

  • 3.

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

Funds: 

National Basic Research Program of China 2014CB440803

National Natural Science Foundation of China 41202046

More Information
  • Author Bio:

    SUN Zhiyuan, male, born in 1989, doctor candidate, majors in mineral resource prospecting and exploration; E-mail:sunzhiyuan010@163.com

  • Received Date: July 15, 2016
  • Revised Date: February 27, 2018
  • Available Online: September 25, 2023
    Graphical Abstract
    • Abstract

  • Marine Na-rich volcanic rocks of Yamansu Formation belong to calc-alkaline series and are dominated by basaltic andesitic porphyrite, andesite, dacite and rhyolite. These volcanic rocks are characterized by low MgO (0.51%-5.93%, averaging 2.54%), FeO (0.54%-6.39%, averaging 2.84%) and TiO2 (0.09%-1.10%, averaging 0.58%) values, high Al2O3 (12.23%-17.75%, averaging 15.2%; A/CNK=0.79-1.42, averaging 1.11), and Na2O (Na2O/K2O 7.30 on average). A majority of plagioclases in the Narich volcanic rocks consist of albite with less oligoclase. Chondrite-normalized REE patterns show the fractionation between LREE and HREE ((LREE/HREE)N=3.68-9.00). The volcanic rocks are also rich in LILE (Th, U, Rb) and depleted in Nb, Ta, Sr, Ti, P. The SHRIMP zircon U-Pb dating yielded (337.6±3.3) Ma. Based on a comparative study of geochemical characteristics and inherited zircon age, the authors hold that Yamansu Na-rich volcanic rocks were formed in an island arc setting with continental basement and were the products of reaction between erupted magma and convective seawater during the subduction of oceanic plate in Early Carboniferous.

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