地形倒置
岩层发生褶曲隆起时，背斜形成山，向斜形成谷。但由于背斜轴部往往张节理比较发育，侵蚀作用进行较快，背斜山可以逐渐演变为背斜谷，而两侧的向斜谷则变成了向斜山。这种地形起伏和构造起伏不一致的现象称为地形倒置(如图)。在软硬岩层相间的褶皱构造区常形成这种地形倒置的现象。
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contributed at 2011-10-11
Classification(s)
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Earth System(in Chinese) Geomorphology
Detailed Description
| English |
|---|
| Name | inverted relief,inversion of relief |
| Chinese |
|---|
| Name | 地形倒置 |
| Description | 岩层发生褶曲隆起时，背斜形成山，向斜形成谷。但由于背斜轴部往往张节理比较发育，侵蚀作用进行较快，背斜山可以逐渐演变为背斜谷，而两侧的向斜谷则变成了向斜山。这种地形起伏和构造起伏不一致的现象称为地形倒置(如图)。在软硬岩层相间的褶皱构造区常形成这种地形倒置的现象。 |
How to Cite
NNU_Group (2011). 地形倒置, Concept & Semantic, OpenGMS,
https://geomodeling.njnu.edu.cn/repository/concept/7f0c618a-919f-40e9-af63-0a45d2342e1a
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