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...
I tiakina i:
| Ngā kaituhi matua: | , , |
|---|---|
| Hōputu: | Artigo |
| Reo: | Inglês |
| I whakaputaina: |
Russian Academy of Sciences, Siberian Branch, Institute of the Earth's crust
2021-03-01
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| Rangatū: | Геодинамика и тектонофизика |
| Ngā marau: | |
| Urunga tuihono: | https://www.gt-crust.ru/jour/article/view/1166 |
| Ngā Tūtohu: |
Kāore He Tūtohu, Me noho koe te mea tuatahi ki te tūtohu i tēnei pūkete!
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