均斜的
The homoclinal reverse fold occurred in the Meso-Proterozoic.The superimposed fold in the late stage occurred in the Early Paleozoic. 主期褶皱形成于中元古代，晚期褶皱形成于早古生代；
The zone sequentially underwent the following stuctural deformations: (1)the tight homoclinal folding at the medium deep tectonic level; 该带依次经历了：（1）中深部构造层次的紧闭同斜褶皱作用；
homoclinal ramp 同斜缓坡
homoclinal valley 单斜谷
