Zobrazeno 1 - 10
of 16
pro vyhledávání: '"N. A. Zakrzhevskaya"'
Publikováno v:
Journal of Volcanology and Seismology. 16:299-310
Publikováno v:
Izvestiya, Physics of the Solid Earth. 57:834-848
Publikováno v:
Izvestiya, Physics of the Solid Earth. 56:291-315
—The response of seismic noise in the minute range of periods to the strong magnetic storms is studied. The noise is analyzed from the records by IRIS broadband seismic stations located in the different regions of the world. The minute variations i
Autor:
Gennady Sobolev, N. A. Zakrzhevskaya
Publikováno v:
Journal of Volcanology and Seismology. 14:137-144
Records of an IRIS broadband seismic station (AAK) deployed in the Tien Shan area were studied. An STS-1 seismometer made it possible to investigate ground motion velocity in the range of a few minutes. The result was to identify asymmetric anomalies
Publikováno v:
Journal of Volcanology and Seismology. 13:1-6
This study is concerned with the behavior of seismic noise in the period range of a few minutes based on records made by broadband IRIS stations before the catastrophic earthquake of March 11, 2011 in Japan. A formalized technique was used to identif
Publikováno v:
Izvestiya, Physics of the Solid Earth. 54:393-405
The records from 161 identical broadband seismic stations located in different regions of the world after the strong earthquakes off Sumatra Island on December 26, 2004 with magnitude M = 9.1, in Chile on February 27, 2010 with M = 8.8, and the Tohok
Publikováno v:
Izvestiya, Physics of the Solid Earth. 53:493-517
The analysis of the records from IRIS broadband seismic stations revealed wave trains with a period of ~129.5 min emerging after the strong earthquakes. These wave trains are simultaneously observed at the stations shifted by 180° in longitude in th
Publikováno v:
Journal of Volcanology and Seismology. 11:103-112
This study is concerned with the influence exerted by worldwide M ≥ 7.5 earthquakes on the seismicity of California, and well as with the effects of M ≥ 5 southern California earthquakes on northern Californian seismicity. The analysis concerns t
Publikováno v:
Izvestiya, Physics of the Solid Earth. 52:155-172
Based on the analysis of the world’s earthquakes with magnitudes M ≥ 6.5 for 1960–2013, it is shown that they cause global-scale coherent seismic oscillations which most distinctly manifest themselves in the period interval of 4–6 min during
Publikováno v:
Izvestiya, Physics of the Solid Earth. 50:474-483
The low-frequency seismic noise recorded by the broadband IRIS stations in 1994–2012 is studied in the period range of 40 to 360 s. It is shown that for samples of a few months in length, the power spectra of noise at stations spaced apart a few th