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Three-dimensional P-velocity model of the mantle and seismicity of Fennoscandia.

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...

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Bibliographic Details
Main Authors: Татьяна Алексеевна Цветкова, Игорь Валентинович Бугаенко, Лариса Николаевна Заец, Tatiana Tsvetkova, Igor Bugaienko, Larysa Zaiets
Format: Article
Language:English
Published: Karelian Research Centre of the Russian Academy of Sciences 2019-02-01
Series:Transactions of the Karelian Research Centre of the Russian Academy of Sciences
Subjects:
трехмерная р-скоростная модель
фенноскандия
мантия
землетрясения
сверхглубинные флюиды three-dimensional p-velocity model
fennoscandia
mantle
earthquakes
super-deep fluids
Online Access:http://journals.krc.karelia.ru/index.php/precambrian/article/view/861
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http://journals.krc.karelia.ru/index.php/precambrian/article/view/861

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