Characteristics and formation mode of salt-bearing series in typical rift valley basin, Eastern China

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• 作者：Yanjun Zhao (1)
  Chenglin Liu (1)
  Hua Zhang (1)
  Licheng Wang (1)
  Baokun Liu (2)
  Fenglin Lv (2)
  
  1. MLR Key Laboratory of Metallogeny and Mineral Assessment ; Institute of Mineral Resources ; CAGS ; Beijing ; 100037 ; China
  2. China University of Geosciences ; Beijing ; 100083 ; China
  
• 关键词：formation mode ; terrigenous detrital ; chemical rock type ; salt ; bearing series ; Shulu Sag ; rift valley
• 刊名：Geosciences Journal
• 出版年：2015
• 出版时间：March 2015
• 年：2015
• 卷：19
• 期：1
• 页码：69-80
• 全文大小：1,185 KB
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• 刊物类别：Earth and Environmental Science
• 刊物主题：Earth sciences
  Geosciences
  
• 出版者：The Geological Society of Korea, co-published with Springer
• ISSN：1598-7477

文摘

The Shulu Sag is a typical rift valley basin in Eastern China, where the formation mechanism of Cenozoic salt-bearing series has been poorly understood. In this paper, petrologic analysis, X-ray powder Diffraction (XRD) analysis and the analysis of halite ion concentrations of the first member of the Shahejie Formation from two drilling cores were conducted to interpret the formation mechanism of these salt-bearing series in Shulu Sag. The results indicated that the salt-bearing series is mainly composed of calcilutite or mudstone at top and bottom, and anhydrite-bearing halite and thin interbeds of salt-bearing calcilutite and dark grey shale in the middle part. These thin interbeds with porphyritic or petalshaped glauberite crystals or some thinner dark grey shale interbeds separated halites into several members with the average thickness of only 9~12 cm in the two drilling holes. This typical rhythmic pattern due to frequent alternation of concentration was evidenced by the variation of chemical composition and hydrogen isotopes of halite fluid inclusions. The presence of large number of primary fluid inclusions within chevron crystals and vertically oriented bottom-growth crystals showed that the halite were precipitated in shallow water (