海进
由于陆地缓慢下降，海水侵入陆地的现象，称为海进。它是在一个相对较短的地质年代中，海域向大陆的扩展，海岸线向陆地移动，导致新的海相岩层超覆在较老的陆相岩层之上，第四纪伴随着间冰期的到来，海面上升常发生海侵。
Classification(s)
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Geographic semantic resource library Earth System(in Chinese) Geology
{{htmlJSON.DetailedDescription}}
| English |
|---|
| Name | transgression |
| Chinese |
|---|
| Name | 海进 |
| Description | 由于陆地缓慢下降，海水侵入陆地的现象，称为海进。它是在一个相对较短的地质年代中，海域向大陆的扩展，海岸线向陆地移动，导致新的海相岩层超覆在较老的陆相岩层之上，第四纪伴随着间冰期的到来，海面上升常发生海侵。 |
{{htmlJSON.HowtoCite}}
NNU_Group (2011). 海进, Concept & Semantic, OpenGMS,
https://geomodeling.njnu.edu.cn/repository/concept/53b36c5b-caee-4725-8d45-dee15cad8b53
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