The Ordovician structure in the middle and east part of the Erdos Basin is a gently west-dipped large monocline. 鄂尔多斯盆地的中东部奥陶系今构造为一平缓的西倾大单斜。
Finally the stratigraphic ages and correlation of the Ordovician lithostratigraphic units in the study area are discussed. 笔者认为,申扎组应被废弃,德悟卡下组底界应作修订,并对该地区奥陶系岩石地层单位进行了简要的时代讨论和对比。