Bulletin of the Seismological Society of America; February 2005; v. 95; no. 1;
p. 1-17; DOI: 10.1785/0120030261
© 2005 Seismological Society of America
Powerful Low-Frequency Vibrators for Active Seismology
A. S. Alekseev1,
I. S. Chichinin2 and
V. A. Korneev3
1 Institute of Computational
Mathematics and Mathematical Geophysics
Siberian Branch of Russian Academy of
Sciences
Lavrentieva pr., 6
630090, Novosibirsk,
Russia
alekseev{at}sscc.ru
(A.S.A.)
2 Institute of Geophysics
Siberian
Branch of Russian Academy of Sciences
Koptuga pr., 3
630090, Novosibirsk,
Russia
iro{at}online.sinor.ru
(I.S.C.)
3 Lawrence Berkeley National
Laboratory
1 Cyclotron Road
Berkeley, California
94720
VAKorneev{at}lbl.gov
(V.A.K.)
In the past two decades, active seismology studies in Russia have made use of
powerful (40- and 100-ton) low-frequency vibrators. These sources create a force
amplitude of up to 100 tons and function in the 1.53, 36, and
510 Hz frequency bands. The mobile versions of the vibrator have a force
amplitude of 40 tons and a 612 Hz frequency band. Recording distances for
the 100-ton vibrator are as large as 350 km, enabling the refracted waves to
penetrate down to 50 km depths. Vibrator operation sessions are highly
repeatable, having distinct "summer" or "winter"
spectral patterns. A long profile of seismic records allows estimation of fault
zone depths using changes in recorded spectra. Other applications include deep
seismic profiling, seismic hazard mapping, structural testing, stress-induced
anisotropy studies, seismic station calibration, and large-structure integrity
testing. The theoretical description of the low-frequency vibrator is given in
the appendices, which contain numerical examples.
Copyright © 2009 by Seismological Society of America