加里东期在东秦岭—大别造山带南侧江汉平原地区存在一个继承性古隆起，前人所称的“鄂中古陆”是其具体的表现。
There is a inherited paleouplift in the Jianghan Plain area of the southern margin of East Qinling and Dabie Orogenic Belt during Caledonian period.
下古生界在加里东运动暴露期间，黔中隆起及周缘盖层化学损失量巨大。
The loss amount of caprocks was huge because of the exposure and chemical erosion during the Caledonian tectonic movements around the upheaval in the middle of Yunnan province.
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