Geodynamic model of upper mantle convection and transformations of the arctic lithosphere in the Mesozoic and Cenozoic

By interpretation of the complex geological and geophysical data and paleotectonic reconstructions based on the results of deep seismic tomography, a new deep geodynamic mechanism is developed to describe the formation and evolution of Amerasian and Eurasian basins, together with their adjacent geol...

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Veröffentlicht in:Izvestiya. Physics of the solid earth 2013-11, Vol.49 (6), p.767-785
Hauptverfasser: Lobkovsky, L. I., Shipilov, E. V., Kononov, M. V.
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container_title Izvestiya. Physics of the solid earth
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creator Lobkovsky, L. I.
Shipilov, E. V.
Kononov, M. V.
description By interpretation of the complex geological and geophysical data and paleotectonic reconstructions based on the results of deep seismic tomography, a new deep geodynamic mechanism is developed to describe the formation and evolution of Amerasian and Eurasian basins, together with their adjacent geological structures of the Arctic region. The Mesozoic and Cenozoic transformations of the lithosphere in a number of regions of the Arctic Ocean are considered. The role and place of the upper-mantle convection is explored, and the chronology of the key structure-forming events is analyzed.
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1555-6506
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source Springer Nature - Complete Springer Journals
subjects Arctic zone
Cenozoic
Convection
Earth and Environmental Science
Earth Sciences
Geological structures
Geology
Geophysics/Geodesy
Lithosphere
Mesozoic
Seismology
Upper mantle
title Geodynamic model of upper mantle convection and transformations of the arctic lithosphere in the Mesozoic and Cenozoic
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