Volume 28 Issue 3
Jun.  2022
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Article Navigation >  Journal of Geomechanics  > 2022  >  28(3): 417-431
MI Jingqiang, CHEN Yuanrong, YU Hao, et al., 2022. Correlation between the distribution characteristics of gallium and sedimentary environment of sedimentary bauxite in Pingguo County, Guangxi, China. Journal of Geomechanics, 28 (3): 417-431. DOI: 10.12090/j.issn.1006-6616.2021090
Citation: MI Jingqiang, CHEN Yuanrong, YU Hao, et al., 2022. Correlation between the distribution characteristics of gallium and sedimentary environment of sedimentary bauxite in Pingguo County, Guangxi, China. Journal of Geomechanics, 28 (3): 417-431. DOI: 10.12090/j.issn.1006-6616.2021090
shu

Correlation between the distribution characteristics of gallium and sedimentary environment of sedimentary bauxite in Pingguo County, Guangxi, China

doi: 10.12090/j.issn.1006-6616.2021090

  • College of Earth Sciences, Guilin University of Technology, Guilin 541000, Guangxi, China

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  • Received: 2021-07-24
  • Revised: 2022-05-16
    Abstract
  • The Pingguo area in Guangxi Province has considerable reserves of sedimentary bauxite of the Upper Permian Heshan Formation which are characterized by the occurrence of associated dispersed element Ga (gallium). It is of great significance to study the geochemical characteristics and depositional environment of the sedimentary bauxite and their correlation with Ga in the deposit on the basis of major and trace element analyses. This research helps to improve the comprehensive recovery and utilization of bauxite, and also to increase the economic values of the deposit. The contents of major and trace elements, including the Ga concentrations, were measured in 18 different types of ores and bauxite samples which were collected in the study area. The results calculated by statistical method and analyzed by correlation diagram show that the average content of Ga in the samples reaches the industrial grade (0.002×10-2), but the enrichment degree of Ga in different ore types accords with the regular rule of oolitic bauxite>dense massive bauxite>aluminous rock. Ga shows a significantly positive lower correlation with Al2O3, but a significantly negative correlation with SiO2, In addition, the Ga concentrations show a slightly positive lower correlation with V and Zr, and no significant correlation with rare earth elements. Based on the analyses of the paleo-geographic environment, Sr/Ba ratios, Ga enrichment and LREE/HREE ratios of different types of samples, this study suggests a costal to shallow marine facies with a relatively stable, acidic and humid climatic condition during the main metallogenic period of the sedimentary bauxite in the Pingguo area. Moreover, an oxidation environment of the coastal facies during the early deposition of the Upper Permian Heshan Formation was gradually transformed into a reducing, shallow marine facies during the late deposition of the Upper Permian Heshan Formation. Correspondingly, the ore type changed from the purplish red, dense massive mineralization to lime gray to grayish dark, oolitic mineralization.

     

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