断陷盆地型岩溶
指断陷盆地内虽有古近新近系及第四系地层分布，但在地下深处，碳酸盐岩岩溶仍较发育。盆地周边地带有较大的岩溶泉及暗河出露，如山西汾河谷地的许多大泉。有的盆地中仍有以岩溶水补给为主的湖泊。云南昆明的滇池就是这种类型的岩溶地貌。
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contributed at 2011-10-12
Classification(s)
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Earth System(in Chinese) Karstology
Detailed Description
| English |
|---|
| Name | faulted basin type karst |
| Chinese |
|---|
| Name | 断陷盆地型岩溶 |
| Description | 指断陷盆地内虽有古近新近系及第四系地层分布，但在地下深处，碳酸盐岩岩溶仍较发育。盆地周边地带有较大的岩溶泉及暗河出露，如山西汾河谷地的许多大泉。有的盆地中仍有以岩溶水补给为主的湖泊。云南昆明的滇池就是这种类型的岩溶地貌。 |
How to Cite
NNU_Group (2011). 断陷盆地型岩溶, Concept & Semantic, OpenGMS,
https://geomodeling.njnu.edu.cn/repository/concept/b47f64ea-ff93-4413-9227-547d498ffbd1
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