Journal of Jilin University(Earth Science Edition) ›› 2018, Vol. 48 ›› Issue (4): 1121-1134.doi: 10.13278/j.cnki.jjuese.20170073

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Rare Earth Element Geochemistry and Genetic Model of Dolomite of Yingshan Formation in Gucheng Area, Tarim Basin

Guo Chuntao1,2, Li Ruyi3, Chen Shumin3   

  1. 1. College of Architecture and Surveying Engineering, Datong University of Shanxi, Datong 037003, Shanxi, China;
    2. Postdoctoral Research Station of Daqing Oilfield Company, Daqing 163453, Heilongjiang, China;
    3. Exploration and Development Research Institute of Daqing Oilfield Company, Daqing 163453, Heilongjiang, China
  • Received:2017-08-21 Online:2018-07-26 Published:2018-07-26
  • Supported by:
    Supported by National Science and Technology Major Project (2016ZX05047-001)

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Abstract: The origin of dolomites is still the hot spot in the geological research. The dolomites of the Yingshan Formation in Gucheng in the Tadong low uplift is discussed in this paper. Based on thin sections and cores, in accordance with the crystal size, the dolomites were divided into five types:micritic, powder crystalline, fine crystalline, medium crystalline, and coarse crystalline dolomites. Meanwhile, the REE geochemical characteristics of various types of dolomites and cave fillings were studied. Based on the results, the NASC(North American average shale) normalized REE distribution patterns of the dolomites and cave fillings in Yingshan Formation showed in the six types:weakly positive anomaly of δCe with positive anomaly δEu, negative anomaly of δCe with heavy positive anomaly δEu, heavy negative anomaly of δCe, tiny right deviation, tiny left deviation, and the flat types. Further, the study showed that the first two kinds of dolomites were formed in a hydrothermal environment; the third kind dolomite was formed in an evaporation pump mode; the fourth and fifth kind dolomites were formed in a buried dolomitizing fluid; and the last kind dolomite was formed in a seepage reflux mode. The dolomite origin of the Yingshan Formation in Gucheng is very complex with various genetic models, including the evaporation pump mode, seepage reflux mode, burial dolomitization mode, and hydrothermal dolomitization mode.

Key words: Gucheng area, Yingshan Formation, dolomite, geochemistry, rare earth element, origin, Tarim basin

CLC Number: 

  • P595
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