Features of seismicity of the Euro-Arctic region
- Авторлар: Rogozhin E.1, Antonovskaya G.2, Kapustian N.1,2, Fedorenko I.2
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Мекемелер:
- Schmidt Institute of Physics of the Earth
- Institute of Ecological Problems of the North, Ural Branch
- Шығарылым: Том 467, № 2 (2016)
- Беттер: 389-392
- Бөлім: Geophysics
- URL: https://journals.rcsi.science/1028-334X/article/view/188276
- DOI: https://doi.org/10.1134/S1028334X16040140
- ID: 188276
Дәйексөз келтіру
Аннотация
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.
Негізгі сөздер
Авторлар туралы
E. Rogozhin
Schmidt Institute of Physics of the Earth
Хат алмасуға жауапты Автор.
Email: eurog@ifz.ru
Ресей, ul. Bolshaya Gruzinskaya 10, Moscow, 123995
G. Antonovskaya
Institute of Ecological Problems of the North, Ural Branch
Email: eurog@ifz.ru
Ресей, Arkhangelsk
N. Kapustian
Schmidt Institute of Physics of the Earth; Institute of Ecological Problems of the North, Ural Branch
Email: eurog@ifz.ru
Ресей, ul. Bolshaya Gruzinskaya 10, Moscow, 123995; Arkhangelsk
I. Fedorenko
Institute of Ecological Problems of the North, Ural Branch
Email: eurog@ifz.ru
Ресей, Arkhangelsk