Tectonic depressions on the East-European and Siberian platforms: numerical modeling of convection beneath the Eurasian continent
In modern concepts, the upper mantle of the Earth is a highly viscous incompressible liquid, and its flow is described using the Navier – Stokes equations in the Oberbeck – Boussinesq and geodynamic approximations. Convective flows in the upper mantle play a decisive role in the kinematics of lithos...
| Main Authors: | , , |
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| Format: | Article |
| Language: | English |
| Published: |
Institute of the Earth's crust, Siberian Branch of RAS
2021-03-01
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| Series: | Geodinamika i Tektonofizika |
| Subjects: | |
| Online Access: | https://www.gt-crust.ru/jour/article/view/1166 |