东部和南部因古老地层褶皱而隆起，形成山地地貌。
As a result of eastern and southern ancient uplift and formation fold, the landscape of mountain formation.
在地壳中一些柔弱地带往往较易受地壳运动剧烈而产生褶皱隆起，而造成绵亘的山脉，世界上许多山脉就是这样形成的。
In the crust some weak areas often more susceptible to intense crustal movement and fold uplift caused by stretching, the mountains, many of the world's mountains is formed.
研究区位于阴山东西向复杂构造带的东段，是与新华夏构造体系大兴安岭褶皱带交接的隆起部位，这种构造为热水的形成、运移奠定了良好的地质环境。
The study area is located in the east of Yinshan with complex structure, joined the Neocathaysian structural system Daxing'anling fold belt at bump contact.
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