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.
红格尔煤田是新华夏系构造体系的产物，断层比较发育。
The Honger coalfield is situated in the Neocathaysian structural system, faults are well developed.
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