岩溶深循环带
在饱水带之下向远方排泄的深部岩溶水带。它受当地排水基准面的影响很弱。并在一定水头压力作用下缓慢径流。深部缓流带可形成深部岩溶，岩溶化程度一般微弱，以溶蚀裂隙和溶孔为主。但在适宜的构造和水质条件下它亦可发育规模巨大的洞穴。
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contributed at 2011-10-12
Classification(s)
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Earth System(in Chinese) Karstology
Detailed Description
| English |
|---|
| Name | karst water deep circulation zone |
| Chinese |
|---|
| Name | 岩溶深循环带 |
| Description | 在饱水带之下向远方排泄的深部岩溶水带。它受当地排水基准面的影响很弱。并在一定水头压力作用下缓慢径流。深部缓流带可形成深部岩溶，岩溶化程度一般微弱，以溶蚀裂隙和溶孔为主。但在适宜的构造和水质条件下它亦可发育规模巨大的洞穴。 |
How to Cite
NNU_Group (2011). 岩溶深循环带, Concept & Semantic, OpenGMS,
https://geomodeling.njnu.edu.cn/repository/concept/d87493ae-6f1d-409a-aaa1-1d050a71abf3
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