There is a inherited paleouplift in the Jianghan Plain area of the southern margin of East Qinling and Dabie Orogenic Belt during Caledonian period.

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。

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Formation and evolution of basins in the southern part of North China are mainly controlled by activities of the Qinling-Dabie orogenic belt and the Tanlu fracture belt.

南华北盆地的形成演化主要受秦岭—大别造山带以及郯庐系断裂带活动的制约。

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