Three-dimensional P-velocity model of the mantle and seismicity of Fennoscandia.
<p>The paper analyzes the three-dimensional P-velocity model of the mantle of North-West Europe (Fennoscandia) in order to isolate the connection of the earth's crustal earthquakes and processes in the mantle. The mantle model was obtained by the Taylor approximation method. This method d...
Main Authors: | , , , , , |
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Format: | Article |
Language: | English |
Published: |
Karelian Research Centre of the Russian Academy of Sciences
2019-02-01
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Series: | Transactions of the Karelian Research Centre of the Russian Academy of Sciences |
Subjects: | |
Online Access: | http://journals.krc.karelia.ru/index.php/precambrian/article/view/861 |