1. Wenlanzhangite–(Y) from the Yushui deposit, South China: A potential proxy for tracing the redox state of ore formation
- Author
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Liu, Peng, Li, Guowu, Sun, Ningyue, Yao, Wei, Yu, Hong, Tian, Yongfei, Yang, Wenqiang, Zhao, Fengshang, and Cook, Nigel J.
- Abstract
Mineral phases in which vanadium (V) and heavy-rare-earth elements (HREEs) coexist are rarely documented. Here, we report a new V-HREE-bearing silicate mineral species, wenlanzhangite-(Y), which is a vanadiferous derivate of jingwenite-(Y) [Y2Al2V24+(SiO4)2O4(OH)4]$\begin{array}{} \displaystyle {\rm [Y_2Al_2V_2^{4+}(SiO_4)_2O_4(OH)_4]} \end{array}$coexisting with jingwenite-(Y) in bedded/massive ores at Yushui, South China. Wenlanzhangite-(Y) forms as a dark brown, 70–100 μm thick rim on a core domain of jingwenite-(Y), which occurs as 100–200 μm columnar crystals. The color, streak, luster, and hardness (Mohs) are dark brown, yellow-gray, vitreous, and ~4, respectively. Compared to jingwenite-(Y), wenlanzhangite-(Y) has higher vanadium and lower aluminum contents. Calculated on the basis of 8 cations, the empirical formula is (Y1.26Dy0.17Er0.11Gd0.09Yb0.09Nd0.09Sm0.06Sc0.04Ho0.03Ce0.02Tb0.02Tm0.02Pr0.01)Σ2.00(V1.463+Al0.54)Σ2.00V24+(SiO4)2O4(OH)4$\begin{array}{} \displaystyle {\rm (V^{3+}_{1.46}Al_{0.54})_{\Sigma2.00}V_2^{4+}(SiO_4)_2O_4(OH)_4} \end{array}$, Which can be simplified to the ideal formula Y2V23+V24+(SiO4)2O4(OH)4$\begin{array}{} \displaystyle {\rm Y_2V_2^{3+}V_2^{4+}(SiO_4)_2O_4(OH)_4} \end{array}$.
- Published
- 2024
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