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KE Xiao-ping, QIN Jian-xiong, LI Yu-sheng, HUANG Ke-nan, LIU Xiu-feng. Characteristics and genesis of the inter-salt dolostones in the Jianghan Basin[J]. Sedimentary Geology and Tethyan Geology, 2009, 29(3): 1-8.
Citation: KE Xiao-ping, QIN Jian-xiong, LI Yu-sheng, HUANG Ke-nan, LIU Xiu-feng. Characteristics and genesis of the inter-salt dolostones in the Jianghan Basin[J]. Sedimentary Geology and Tethyan Geology, 2009, 29(3): 1-8.
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Characteristics and genesis of the inter-salt dolostones in the Jianghan Basin

  • 1. Institute of Geodesy and Geophysics, Chinese Academy of Sciences, Wuhan 430077, Hubei, China;

  • 2. Institute of Sedimentary Geology, Chengdu University of Technology, Chengdu 610059, Sichuan, China;

  • 3. Research Institute of Petroleum Exploration and Development, Jianghan Oil Field Company, SINOPEC, Qianjiang 433124, Hubei, China

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  • Published Date: September 29, 2009
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    • Abstract
  • A succession of inter-salt non-sandstones occurs on a wide range of scales in the Palaeogene Qianjiang Formation in the Qianjiang depression,Jianghan salt lake basin.The present paper deals,in detail,with the distribution,type,mineralogy,geochemistry and genesis of the dolostones in the inter-salt non-sandstones from the basin.The inter-salt dolostones dominated by micritic dolostones are characterized by complex mineral compositions,lower ordering degree,rich Fe and Na and high Fe/Mn ratios,and thus interpreted as the products deposited in the sedimentary environment of salt lake basin during the primary-penecontemporaneous stages.
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