Email this article Features of seismicity of the Euro-Arctic region
- Authors: Rogozhin E.A.1, Antonovskaya G.N.2, Kapustian N.K.1,2, Fedorenko I.V.2
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Affiliations:
- Schmidt Institute of Physics of the Earth
- Institute of Ecological Problems of the North, Ural Branch
- Issue: Vol 467, No 2 (2016)
- Pages: 389-392
- Section: Geophysics
- URL: https://bakhtiniada.ru/1028-334X/article/view/188276
- DOI: https://doi.org/10.1134/S1028334X16040140
- ID: 188276
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Abstract
New results from seismic monitoring in the Euro-Arctic region, including the seismicity of Gakkel Ridge and the Barents–Kara Sea shelf, are presented. The data used were obtained from the Arkhan-gelsk seismic network. The role of island-based seismic stations, in particular, those in Franz Josef Land, in the monitoring network is discussed. The possibility of specifying the nature of seismicity by waveform spectral-temporal analysis, even in the case of a single station, is considered.
About the authors
E. A. Rogozhin
Schmidt Institute of Physics of the Earth
Author for correspondence.
Email: eurog@ifz.ru
Russian Federation, ul. Bolshaya Gruzinskaya 10, Moscow, 123995
G. N. Antonovskaya
Institute of Ecological Problems of the North, Ural Branch
Email: eurog@ifz.ru
Russian Federation, Arkhangelsk
N. K. Kapustian
Schmidt Institute of Physics of the Earth; Institute of Ecological Problems of the North, Ural Branch
Email: eurog@ifz.ru
Russian Federation, ul. Bolshaya Gruzinskaya 10, Moscow, 123995; Arkhangelsk
I. V. Fedorenko
Institute of Ecological Problems of the North, Ural Branch
Email: eurog@ifz.ru
Russian Federation, Arkhangelsk
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