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Publikováno v:
Zhongguo dizhi zaihai yu fangzhi xuebao, Vol 32, Iss 2, Pp 43-52 (2021)
Most of the soluble rocks in Wuhan lie in the quaternary soil layer and the lower part of the chalk-paleogene red layer, the geological structure of the distribution area of soluble rock is closely related to the karst ground collapse, most of the ha
Externí odkaz:
https://doaj.org/article/16fd7f778a1f4118a99cf1cd9638a454