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

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...

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Bibliographic Details
Main Authors: L. I. Lobkovsky, M. M. Ramazanov, V. D. Kotelkin
Format: Article
Language:English
Published: Russian Academy of Sciences, Siberian Branch, Institute of the Earth's crust 2021-09-01
Series:Геодинамика и тектонофизика
Subjects:
lithosphere
subduction zone
upper mantle
thermal convection
2d convection model
3d modeling
cretaceous-cenozoic evolution
central east asia
arctic
baikal rift zone
Online Access:https://www.gt-crust.ru/jour/article/view/1234
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