LI Xin, CAO Hong, GENG Wei, SUN Zhilei, ZHANG Xilin, YAN Dawei, QIN Shuangshuang, XU Cuiling, ZHANG Xianrong, ZHAI Bin, WANG Libo. Research progress in carbonate associated sulfate[J]. Marine Geology & Quaternary Geology, 2020, 40(3): 119-131. DOI: 10.16562/j.cnki.0256-1492.2019090801
Citation: LI Xin, CAO Hong, GENG Wei, SUN Zhilei, ZHANG Xilin, YAN Dawei, QIN Shuangshuang, XU Cuiling, ZHANG Xianrong, ZHAI Bin, WANG Libo. Research progress in carbonate associated sulfate[J]. Marine Geology & Quaternary Geology, 2020, 40(3): 119-131. DOI: 10.16562/j.cnki.0256-1492.2019090801

Research progress in carbonate associated sulfate

  • Carbonate associated sulfate, or CAS in brief, is one of the important indicators for paleoenvironmental restoration. Trace sulfate may enter carbonate lattice and replaces the carbonate during diagenesis. The CAS has the capability to preserve the isotopic composition of seawater sulfate and to record the sulfate concentration of seawater, as well as the changes in the paleoenvironment. In recent years, CAS has attracted great interest and attention from the geological society. In this paper, attempt has been made to address CAS with emphases on its pre-treatment methods, influencing factors, isotopic composition and its significance in paleoenvironmental reconstruction. The application of CAS to the restoration of different sedimentary environments is discussed, in addition to the future research directions. We hope that the introduction may raise interests and attentions from researchers.
  • loading

Catalog

    Turn off MathJax
    Article Contents

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return