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ON HEAT SOURCE IN SUBDUCTION ZONE
The subduction of an oceanic plate is studied as the motion of a high-viscosity Newtonian fluid. The subducting plate spreads along the 670-km depth boundary under the influence of oppositely directed horizontal forces. These forces are due to oppositely directed horizontal temperature gradients. We...
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| Main Authors: | , , , |
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| Formato: | Artigo |
| Idioma: | Inglês |
| Publicado em: |
Institute of the Earth's crust, Siberian Branch of RAS
2021-09-01
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| Colecção: | Geodinamika i Tektonofizika |
| Assuntos: | |
| Acesso em linha: | https://www.gt-crust.ru/jour/article/view/1235 |
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