Localization of Geological Inhomogeneities on the Arctic Shelf by Analysis of the Seismoacoustic Wave Field Mode Structure
- Авторлар: Sobisevich A.L.1, Presnov D.A.1, Sobisevich L.E.1, Shurup A.S.1,2
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Мекемелер:
- Schmidt Institute of Physics of the Earth
- Department of Physics
- Шығарылым: Том 479, № 1 (2018)
- Беттер: 355-357
- Бөлім: Geophysics
- URL: https://ogarev-online.ru/1028-334X/article/view/192503
- DOI: https://doi.org/10.1134/S1028334X18030108
- ID: 192503
Дәйексөз келтіру
Аннотация
The results of analysis of wave modes in the ambient noise induced in the layered structure “lithosphere–hydrosphere–ice sheet” are presented. It is shown that instrumental monitoring over background noises in an ice-covered shallow sea allows us to apply methods of seismic tomography in order to determine the structural parameters of a layered geophysical media.
Авторлар туралы
A. Sobisevich
Schmidt Institute of Physics of the Earth
Email: presnov@physics.msu.ru
Ресей, Moscow, 123242
D. Presnov
Schmidt Institute of Physics of the Earth
Хат алмасуға жауапты Автор.
Email: presnov@physics.msu.ru
Ресей, Moscow, 123242
L. Sobisevich
Schmidt Institute of Physics of the Earth
Email: presnov@physics.msu.ru
Ресей, Moscow, 123242
A. Shurup
Schmidt Institute of Physics of the Earth; Department of Physics
Email: presnov@physics.msu.ru
Ресей, Moscow, 123242; Moscow, 119991
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