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WANG Jie, KANG Lei, YANG Xuanjiang, ZHANG Chenbo, ZU Qian, ZHAN Haipeng, LI Ling, YONG Huahua. 2025. Discovery and geological significance of the Late Carboniferous volcanic edifices in Baishan of Southern Beishan area, Xinjiang. East China Geology, 46(2): 222-237. doi: 10.16788/j.hddz.32-1865/P.2024.01.017
Citation: WANG Jie, KANG Lei, YANG Xuanjiang, ZHANG Chenbo, ZU Qian, ZHAN Haipeng, LI Ling, YONG Huahua. 2025. Discovery and geological significance of the Late Carboniferous volcanic edifices in Baishan of Southern Beishan area, Xinjiang. East China Geology, 46(2): 222-237. doi: 10.16788/j.hddz.32-1865/P.2024.01.017
shu

Discovery and geological significance of the Late Carboniferous volcanic edifices in Baishan of Southern Beishan area, Xinjiang

  • 1.

    Northwest Nonferrous Engineering Co., Lth, Xi’an 710038, Shaanxi, China

  • 2.

    Xi’an Center, China Geological Survey, Xi’an 710119, Shaanxi, China

  • 3.

    Chengdu University of Technology, Chengdu610059, Sichuan, China

More Information
Received Date:  17 January 2024
Revised Date:  29 November 2024
Accepted Date:  29 November 2024
Publish Date:  28 June 2025
    Abstract

  • There are lesser research on when the Late Paleozoic rift belt of the Beishan area began to rift. A complete volcanic edifice is identified in the southern Beishan rift belt through 1∶50 000 regional geological survey. The rock association is composed of andesite, dacite, basalt, rhyolite and pyroclastic rocks with the zircon U-Pb age ranging between 313～300 Ma.The volcanic rocks are characterized with high NaO2 and Mg#, low CaO and TiO2, belonging to calc-alkaline series. The REE pattern is distributed in obvious right-tendency with little depletion of Eu (δEu=0.72～1.00), enriched in large ion lithophile elements Rb, Th, K and LREE, and depleted in Nb, Ta, P and Ti. Based on the geochemical characteristics of rocks and key indices such as (Th/Nb)N and (Nb/La)N, it indicates that the volcanic rocks were intensely mixed with crust materials during the magma eruption. The sedimentary sequence in clastic rocks infers that it should be formed in an intra-continental environment. Diagrams of Zr/Nb-Nb/Th and Zr/Y-Nb/Y show that the basic volcanic rocks may derived from the tectonic environment associated with mantle plumes. Based on the diagram of Zr/Y-Zr and Th/Hf-Ta/Hf, in combination with the regional geological characteristics, the authors consider that the volcanic rocks might occur in the initial cracking environment of continental rift. This is the earliest age-information of the rift zone reported so far, which indicates that the southern Beishan area has initially entered in the intracontinental initial rift environment in the Late Carboniferous.

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