基于以上原因，砂泥岩组合型式对异常超压带的发育有重要影响。
Due to the above reason the association of sandstone and mudstone is important to the form of abnormal pressure zones.
砂泥岩组合方式在不同埋深条件下影响了砂泥岩界面附近储层的物性。
Porosity and permeability of sandstone near the sandstone-mudstone boundary is affected by the stacking pattern of sandstone and mudstone.
与砂泥岩地层相比，碳酸盐岩地层常以高电阻率、深浅双侧向大幅度差异为特征。
Carbonate formation is characterized by higher resistivity and bigger difference of Dual and Shallow lateral logging compared with clastic formation.
应用推荐