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CHEN Bingfang, LIN Wenshan, BAI Jianhai, et al. Geological Characteristics and Genetic Analysis of the Jiandingshan Strontium Deposit in Western Qaidam Basin[J]. Northwestern Geology, 2018, 51(4): 184-193.
Citation: CHEN Bingfang, LIN Wenshan, BAI Jianhai, et al. Geological Characteristics and Genetic Analysis of the Jiandingshan Strontium Deposit in Western Qaidam Basin[J]. Northwestern Geology, 2018, 51(4): 184-193.
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Geological Characteristics and Genetic Analysis of the Jiandingshan Strontium Deposit in Western Qaidam Basin

  • 1. Qinghai Provincial Key Laboratory of Geological Processes and Mineral Resources of Northern Qinghai-Tibetan Plateau, Qinghai Institute of Geological Survey, Xining 810012, Qinghai, China;

  • 2. Qinghai Province Third Geological and Mineral Exploration Institute, Xining 810001, Qinghai, China

More Information
  • Received Date: April 16, 2018
  • Revised Date: May 27, 2018
  • Available Online: July 28, 2022
  • Published Date: December 04, 2018
    Graphical Abstract
    • Abstract
  • The Jiandingshan celestite deposit is located in the northwestern margin of the Qaidam Basin. The orebodies are mainly situated with layered, layered, lenticular shapes in calcareous mudstone containing carbon and limestone from the upper member of Pliocene Shizigou group. Orebody is mainly composed of native celestite, with high grade and good spatial continuity. Ore-bearing sandstone has lower ΣREE value with an average value of 42.73×10-6, its LREE/HREE ratio is 6.48, and δEu (0.94) and δCe (0.98) slightly negative anomaly. La/Yb-REE Plots denote that the ore-forming materials were derived from multiple sources with a main contribution from sedimentary rocks. The fluids for celestine formation might be derived from underground brine and peripheral continental basin. In summary, it's believed that this deposit may be had the characteristics of terrestrial detrital chemical deposition.
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    • References (45)
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