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    Volume 47 Issue 4
    Apr.  2022
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    Li Zhidan, Li Shanpo, Guo Hu, Zeng Wei, Cui Yurong, Li Xiaoguang, Chen Junkui, Zhang Shaobo, 2022. Geochemical, U-Pb Age and Nd-Isotopic Characteristics of Titanite in Alkaline Rocks from Dazhuang Nb-REE Deposit in Southern Margin of North China Craton. Earth Science, 47(4): 1415-1434. doi: 10.3799/dqkx.2021.126
    Citation: Li Zhidan, Li Shanpo, Guo Hu, Zeng Wei, Cui Yurong, Li Xiaoguang, Chen Junkui, Zhang Shaobo, 2022. Geochemical, U-Pb Age and Nd-Isotopic Characteristics of Titanite in Alkaline Rocks from Dazhuang Nb-REE Deposit in Southern Margin of North China Craton. Earth Science, 47(4): 1415-1434. doi: 10.3799/dqkx.2021.126

    Geochemical, U-Pb Age and Nd-Isotopic Characteristics of Titanite in Alkaline Rocks from Dazhuang Nb-REE Deposit in Southern Margin of North China Craton

    doi: 10.3799/dqkx.2021.126
    • Received Date: 2021-06-11
      Available Online: 2022-04-29
    • Publish Date: 2022-04-25
    • The Dazhuang deposit is a newly discovered medium-scale Nb-REE deposit which is located at the Fangcheng County of Henan Province on the southern margin of the North China craton. The Nb-REE orebodies are hosted in biotite syenite and hornblende nepheline syenite of Neoproterozoic Shuangshan alkaline pluton. In this paper, major and trace elements, U-Pb geochronology and in-situ Nd isotope studies were carried out on the titanite from the alkaline rocks by EPMA and LA-ICP-MS. The average contents of SiO2 (28.597%-31.169%), CaO (25.492%-28.949%) and TiO2 (34.126%-38.940%) in titanite are significantly lower than the theoretical values, whereas it contains relatively high contents of F (0.141%-1.086%), Al2O3 (1.573%-2.817%) and FeO (0.446%-2.147%). The titanite in Dazhuang deposit has a very high total amount of REE (∑REE=781.47×10-6-31 766.59×10-6). In the chondrite-normalized REE patterns, the rare earth distribution curve is obviously right-leaning, and the light and heavy rare earth fractionation is obvious. There are obvious negative δEu anomalies (0.27-0.86) and inconspicuous δCe anomalies (0.97-1.22), with Th/U values ranging from 1.40 to 11.86, suggesting that the titanite is magmatic origin. The formation temperature of Dazhuang alkaline rocks obtained by the titanite Zr thermometer is 667-964 ℃, with an average of 933 ℃. The titanite in Dazhuang deposit has very high Nb and REE contents, indicating that the titanite is an important ore-bearing mineral, and the Nb and REE are the result of the gradual enrichment of magma evolution. Formation ages of 848±35 Ma, 849±22 Ma, 843±30 Ma, 845±20 Ma, 845±24 Ma, and 849±40 Ma were obtained from the Nb-rich titanite samples, constraining that the mineralization age of Dazhuang Nb-REE deposit is Neoproterozoic, of which related to the breakup of the Rodinia supercontinent. Titanite has a relatively uniform Nd isotope (εNd(t)=-3.25 to -0.66) value, indicating that the original magma was derived from mantle where rich in phlogopite.

       

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