岩溶断块山地
又称岩溶块状山。是发育在断裂错动上升区的岩溶地形。常见于新生代差异性升降运动强烈的区域。断块山地之间，有的地方是断陷盆地。山地多呈条状或块状分布，边缘为断层，山地方向与断层走向近一致，断崖悬立、岩石裸露，相对高差常达500～1000米以上。
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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 fault block mountain |
| Chinese |
|---|
| Name | 岩溶断块山地 |
| Description | 又称岩溶块状山。是发育在断裂错动上升区的岩溶地形。常见于新生代差异性升降运动强烈的区域。断块山地之间，有的地方是断陷盆地。山地多呈条状或块状分布，边缘为断层，山地方向与断层走向近一致，断崖悬立、岩石裸露，相对高差常达500～1000米以上。 |
How to Cite
NNU_Group (2011). 岩溶断块山地, Concept & Semantic, OpenGMS,
https://geomodeling.njnu.edu.cn/repository/concept/d5d8d37f-f0ec-4f11-9cc9-5580453917b3
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