Features of seismicity of the Euro-Arctic region


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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.

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E. Rogozhin

Schmidt Institute of Physics of the Earth

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Email: eurog@ifz.ru
俄罗斯联邦, ul. Bolshaya Gruzinskaya 10, Moscow, 123995

G. Antonovskaya

Institute of Ecological Problems of the North, Ural Branch

Email: eurog@ifz.ru
俄罗斯联邦, Arkhangelsk

N. Kapustian

Schmidt Institute of Physics of the Earth; Institute of Ecological Problems of the North, Ural Branch

Email: eurog@ifz.ru
俄罗斯联邦, ul. Bolshaya Gruzinskaya 10, Moscow, 123995; Arkhangelsk

I. Fedorenko

Institute of Ecological Problems of the North, Ural Branch

Email: eurog@ifz.ru
俄罗斯联邦, Arkhangelsk

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