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UPPER MANTLE CONVECTION RELATED TO SUBDUCTION ZONE AND APPLICATION OF THE MODEL TO INVESTIGATE THE CRETACEOUS-CENOZOIC GEODYNAMICS OF CENTRAL EAST ASIA AND THE ARCTIC
A geodynamic model of upper mantle convection related to the Pacific subduction zone is mathematically substantiated and applied to investigate the Cretaceous-Cenozoic evolution of Central East Asia (CEA) and the Arctic. We present a solution for the two-dimensional stationary problem of thermal con...
Wedi'i Gadw mewn:
Prif Awduron: | , , |
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Fformat: | Artigo |
Iaith: | Inglês |
Cyhoeddwyd: |
Institute of the Earth's crust, Siberian Branch of RAS
2021-09-01
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Cyfres: | Geodinamika i Tektonofizika |
Pynciau: | |
Mynediad Ar-lein: | https://www.gt-crust.ru/jour/article/view/1234 |
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