Advanced Search
    CAO Ying-chang, WANG Zhu-kun, WANG Yan-zhong, LI Yu-zhi, ZHAO Bo. Architectures and responses of physical properties of the unconformity in the uppermost part of the Palaeogene strata in the Yongbei region, Dongying depression[J]. Sedimentary Geology and Tethyan Geology, 2016, 36(3): 98-103.
    Citation: CAO Ying-chang, WANG Zhu-kun, WANG Yan-zhong, LI Yu-zhi, ZHAO Bo. Architectures and responses of physical properties of the unconformity in the uppermost part of the Palaeogene strata in the Yongbei region, Dongying depression[J]. Sedimentary Geology and Tethyan Geology, 2016, 36(3): 98-103.

    Architectures and responses of physical properties of the unconformity in the uppermost part of the Palaeogene strata in the Yongbei region, Dongying depression

    • The architectures and responses of physical properties of the unconformity are discussed according to the 3-D seismic data, thin section examination, well logs and physical properties of the unconformity at the uppermost part of the Palaeogene strata in the Yongbei region, Dongying depression. The three-layer architectures are discriminated for the unconformity, including the transgressive sand layer with high porosity, weathered clay layer with higher mud contents and lower porosity, and semi-weathered leached layer with developed secondary opening solutions and higher porosity. There occur two types of stratigraphic traps such as the block-tilting and basin-margin types developed in the upper part of the third member of the Shahejie Formation in the Yongbei region. The blocktilting model is controlled by the unconformity and second-order or lower-order faults, and thus displays relatively small scales of traps. The basin-margin model often appears on the highly-uplifted basin margins constrained by the faults, and thus display relatively larger scales of traps.
    • loading

    Catalog

      Turn off MathJax
      Article Contents

      /

      DownLoad:  Full-Size Img  PowerPoint
      Return
      Return