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...

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Hauptverfasser:	V. V. Chervov, N. A. Bushenkova, G. G. Chernykh
Format:	Artigo
Sprache:	Inglês
Veröffentlicht:	Russian Academy of Sciences, Siberian Branch, Institute of the Earth's crust 2021-03-01
Schriftenreihe:	Геодинамика и тектонофизика
Schlagworte:	thermal convection mathematical modeling mantle lithosphere thickness craton depression syneclise platform
Online-Zugang:	https://www.gt-crust.ru/jour/article/view/1166
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