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Volume 37 Issue 2
Apr 2026
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Ying Wang, Cuicui Wang, Zuohuai Yang, Lei Jiang. Petrogenesis and Nb Metallogenic Implications of the Yilan-Like Rare-Metal-Bearing Peralkaline-Alkaline Intrusion in the Northern Tarim Basin in Northwest China. Journal of Earth Science, 2026, 37(2): 484-507. doi: 10.1007/s12583-024-0091-3
Citation: Ying Wang, Cuicui Wang, Zuohuai Yang, Lei Jiang. Petrogenesis and Nb Metallogenic Implications of the Yilan-Like Rare-Metal-Bearing Peralkaline-Alkaline Intrusion in the Northern Tarim Basin in Northwest China. Journal of Earth Science, 2026, 37(2): 484-507. doi: 10.1007/s12583-024-0091-3

Petrogenesis and Nb Metallogenic Implications of the Yilan-Like Rare-Metal-Bearing Peralkaline-Alkaline Intrusion in the Northern Tarim Basin in Northwest China

doi: 10.1007/s12583-024-0091-3
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  • Corresponding author: Cuicui Wang, wcc7011@126.com
  • Received Date: 22 May 2024
  • Accepted Date: 11 Nov 2024
  • Available Online: 30 Mar 2026
  • Issue Publish Date: 30 Apr 2026
  • Despite extensive studies on Nb deposits associated with alkaline rocks, the key factors controlling Nb enrichment remain uncertain, with conditions varying across distinct alkaline intrusions. To better understand Nb mineralization in alkaline rocks, we conducted an integrated investigation of samples from an Nb-bearing peralkaline-alkaline intrusion in the Yilan-like region of the northern Tarim Basin. The Yilan-like intrusion is predominatly composed of granitic pegmatite, alkali pegmatite, syenite, and sodalite syenite. Zircon dating results reveal that this intrusion was emplaced at about 276 Ma. The Yilan-like intrusion is characterized by high SiO2 and total alkali contents and prominent enrichment of HFSE and LREE, with obvious depletions of Ba, K, P, and Ti. The peralkaline-alkaline rocks have high initial 87Sr/86Sr ratios (0.715 8 to 0.853 3) and negative εNd(t) values (-7.8 to -8.5). We propose that the Yilan-like peralkaline-alkaline intrusion was generated via remelting of deep crustal materials enriched in alkali, F, and HFSE. With Nb concentrations reaching up to 252 ppm and Nb primarily hosted in titanite, ilmenite, rutile, pyrochlore, and columbite, the intrusion shows significant potential for Nb mineralization. Based on the chemical compositions of Nb minerals, we suggest that both magmatic and hydrothermal processes played key roles in Nb enrichment.

     

  • Electronic Supplementary Material: Supplementary material (Table S1) is available in the online version of this article at https://doi.org/10.1007/s12583-024-0091-3.
    Conflict of Interest
    The authors declare that they have no conflict of interest.
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