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SHI Hao, QIN Xiaofeng, WANG Zongqi, et al. Geological, Geochemical Characteristics and Genetic Information of the Lijiawan Manganese Deposit in Songtao Area, East Guizhou[J]. Northwestern Geology, 2019, 52(1): 109-122. DOI: 10.19751/j.cnki.61-1149/p.2019.01.010
Citation: SHI Hao, QIN Xiaofeng, WANG Zongqi, et al. Geological, Geochemical Characteristics and Genetic Information of the Lijiawan Manganese Deposit in Songtao Area, East Guizhou[J]. Northwestern Geology, 2019, 52(1): 109-122. DOI: 10.19751/j.cnki.61-1149/p.2019.01.010
shu

Geological, Geochemical Characteristics and Genetic Information of the Lijiawan Manganese Deposit in Songtao Area, East Guizhou

  • 1. Guangxi Key Laboratory of Hidden Metallic Ore Deposits Exploration, College of Earth Science, Guilin University of Technology, Guilin 541004, Guangxi, China;

  • 2. China Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China

More Information
  • Received Date: March 11, 2018
  • Revised Date: October 08, 2018
  • Available Online: July 28, 2022
  • Published Date: March 04, 2019
    Graphical Abstract
    • Abstract
  • The Lijiawan manganese deposit is one of the typical "Datangpo type" deposits in Songtao area of Guizhou province, which is a large concealed type manganese deposit disicovered in recent years and is also the deep peripheral extension of the Yanglizhang manganese ore bodies. Based on the field geological investigation, this paper focuses on the study of the geological, geochemical characteristics and its surrounding rocks of this manganese deposit, and then the ore-forming sources, genetic and mineralized environment of this deposit have been discussed. The results show that the ores occurred as massive, banded and mottled types, with mainly manganese minerals of rhodochrosite and greinerite. The content manganese layer has high MnO, CaO and MgO contents, but it has low TiO2, Al2O3, K2O and Na2O contents, and the manganese-bearing rock series are enriched in Ba, Th, Rb, Cs, Zr, Cs and Ga elements. The SiO2/Al2O3 ratio shows the materials were not sourced from normal terrigenous;The Al/(Al+Fe+Mn), (Fe+Mn)/Ti, Fe/Ti, Y/Ho, Nb/Ta and U/Th ratios, Fe-Mn-(Cu+Co+Ni) * 10 diagram show that the manganese ore has hydrothermal sedimentary characteristics;The Mn/Fe, Sr/Ba, V/(V+Ni) ratios reveal that the manganese ore was formed in shallow water and reductive sedimentary environment. The total REE is higher, with LREE enrichment;The manganese-bearing rock series have Eu and Ce anomalies;The La/Ce ratio, the REE and HREE values reflecct that the manganese deposition process was effected by hydrothermal activity, with a tectonic environment of passive continental margin. According to the characteristics mentioned above, it's included that the Lijiawan manganese deposit was formed in strong reducing environment, which was sourced from the mixing of hydrothermal and normal deposition.
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