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鄂西一带的区域地质研究,迄今已有三十余年的历史,亦累积了一些珍贵的资料。学者们一致认为本地区自雪峰运动之后,虽然经历过多次地壳运动,但这些地壳运动在本地区表现的均为振荡性质的升降作用和一些微弱的弯曲作用。虽然亦相应地发生沉积中断,但往往是经历时间较短并且亦限于局部地区。中生代末期燕山运动改变了本地区的自然面貌,使所有沉积岩褶皱成山,嗣后就长期遭受剥蚀、侵触作用直到目前。在剥蚀作用过程中,各时代被褶皱的石灰岩相
The study of regional geology in western Hubei has so far accumulated more than thirty years of history and accumulated some valuable information. The scholars agreed that although the region experienced many crustal movements since the snow-capped peaks, these crustal movements showed oscillatory movements and some weak bending effects in the region. Although sedimentary disruptions also occur accordingly, they tend to be short-lived and limited to localized areas. The Yanshan movement at the end of the Mesozoic Era has changed the natural landscape of the area, causing all the sedimentary rocks to fold into mountains and later suffered long-term erosion and invasion until now. In the denudation process, the limestone facies were folded in all ages