俯冲带
岩石圈板块被迫向下进入或消减于软流圈的一个区域，岩石圈板块运动是岛弧区域发生地震的原因。当它向下进入地幔时，板块被加热，并在100～300km深处被部分熔化，在700km深处则完全熔化。
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contributed at 2011-12-23
Classification(s)
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Earth System(in Chinese) Geology
Detailed Description
| English |
|---|
| Name | subduction zone |
| Chinese |
|---|
| Name | 俯冲带 |
| Description | 岩石圈板块被迫向下进入或消减于软流圈的一个区域，岩石圈板块运动是岛弧区域发生地震的原因。当它向下进入地幔时，板块被加热，并在100～300km深处被部分熔化，在700km深处则完全熔化。 |
How to Cite
NNU_Group (2011). 俯冲带, Concept & Semantic, OpenGMS,
https://geomodeling.njnu.edu.cn/repository/concept/b12bb150-fe2d-4949-af4d-0478bbc2d2b8
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