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WANG Zheng-jiang, GUO Ting-ting, YU Sai-ying, CHENG Yan-xun, ZHANG Chun-bo, ZHANG Yu-dong. Geochemistry and provenance analysis of the Daheishan bauxite deposit in Huize, Yunnan[J]. Sedimentary Geology and Tethyan Geology, 2016, 36(1): 23-29.
Citation: WANG Zheng-jiang, GUO Ting-ting, YU Sai-ying, CHENG Yan-xun, ZHANG Chun-bo, ZHANG Yu-dong. Geochemistry and provenance analysis of the Daheishan bauxite deposit in Huize, Yunnan[J]. Sedimentary Geology and Tethyan Geology, 2016, 36(1): 23-29.
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Geochemistry and provenance analysis of the Daheishan bauxite deposit in Huize, Yunnan

  • 1. Faculty of Land and Resource Engineering, Kunming University of Science and Technology, Kunming 650093, Yunnan, China;

  • 2. Yunnan Institute of Geological Survey, Kunming 650216, Yunnan, China;

  • 3. No. 10 Gold Exploration Party, Chinese Armed Police Force, Kunming 637350, Yunnan, China

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  • Received Date: August 01, 2015
  • Revised Date: October 11, 2015
  • Published Date: March 29, 2016
    Graphical Abstract
    • Abstract
  • The Daheishan bauxite deposit in Huize, Yunnan resides in the basal part of the Upper Permian Xuanwei Formation underlain by the Emeishan basalts. The bauxite ores from the Daheishan deposit display micritic, oolitic and granular textures, and densely massive, stratified and stratoid structures. There are both negative correlations between Al2O3 and Fe2O3, and Al2O3 and SiO2 and good correlations between TiO2 and Zr, Hf, Nb and Ta, Zr and Hf, Nb and Ta. The bauxite and basalt samples in this study exhibit similar normalized distribution patterns. The ore-forming matter may be derived from the underlying Emeishan basalts, as indicated by LogNi and LogCr diagram.
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