地震陡坎
由于地震断层和地震地表破裂带两侧差异升降运动形成的、由一个倾向下降盘的自由面组成的线状陡坎或陡崖；发育在第四纪沉积物中的断层陡坎由上原始面、自由面(随陡坎演化而消失)、冲刷坡、碎屑坡、下原始面等基本微地貌单元组成，其剖面的演化特征可以指示断层重复错动的期次、位移量、相对年代等。
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contributed at 2011-10-13
Classification(s)
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Earth System(in Chinese) Earthquake geology
Detailed Description
| English |
|---|
| Name | earthquake scarp |
| Chinese |
|---|
| Name | 地震陡坎 |
| Description | 由于地震断层和地震地表破裂带两侧差异升降运动形成的、由一个倾向下降盘的自由面组成的线状陡坎或陡崖；发育在第四纪沉积物中的断层陡坎由上原始面、自由面(随陡坎演化而消失)、冲刷坡、碎屑坡、下原始面等基本微地貌单元组成，其剖面的演化特征可以指示断层重复错动的期次、位移量、相对年代等。 |
How to Cite
NNU_Group (2011). 地震陡坎, Concept & Semantic, OpenGMS,
https://geomodeling.njnu.edu.cn/repository/concept/5898d5e7-cb22-4633-b3ff-1806fa34b1fe
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