RUSSIAN JOURNAL OF EARTH SCIENCES, VOL. 12, ES5003, doi:10.2205/2012ES000522, 2012


Figure 4. Signal with TW-disturbance, starts at the point $i\approx 6,706,750$.


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Citation: Getmanov V. G. (2012), Method of spectral-time analysis for recognition of anomalies in time series with Raleigh- and tsunami-wave disturbances in signals from hydrostatic pressure sensors of ocean bottom seismic stations, Russ. J. Earth Sci., 12, ES5003, doi:10.2205/2012ES000522.


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