海积夷平岸
使海岸因堆积作用而夷平的海岸。在海水淹没的平原上，由于海岸带物质来源多，水下岸坡平缓，海岸以堆积作用为主，在水下岸坡下部冲刷产物沿岸坡上移，形成水下堤、离岸堤、海滩等。其不同发育阶段，在中国渤海湾西岸、苏北海岸、台湾省西岸都有分布。
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contributed at 2011-10-13
Classification(s)
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Earth System(in Chinese) Marine geology
Detailed Description
| English |
|---|
| Name | coast leveled by marine accumulation |
| Chinese |
|---|
| Name | 海积夷平岸 |
| Description | 使海岸因堆积作用而夷平的海岸。在海水淹没的平原上，由于海岸带物质来源多，水下岸坡平缓，海岸以堆积作用为主，在水下岸坡下部冲刷产物沿岸坡上移，形成水下堤、离岸堤、海滩等。其不同发育阶段，在中国渤海湾西岸、苏北海岸、台湾省西岸都有分布。 |
How to Cite
NNU_Group (2011). 海积夷平岸, Concept & Semantic, OpenGMS,
https://geomodeling.njnu.edu.cn/repository/concept/2041eb22-8445-489b-9a35-0a591a155011
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