RUSSIAN JOURNAL OF EARTH SCIENCES, VOL. 17, ES1003, doi:10.2205/2017ES000591, 2017
Figure 2. The results of geoacoustic measurements in different frequency channels in the time vicinity of the earthquake swarm in October 2001, the G-1 borehole, depth 1035 m, $Z$-component: (a) – time series of the water discharge of the GK-1 borehole; (b) – the rms GAE time series for the 160-Hz frequency channel; (c) – the rms GAE time series for the 1200-Hz channel; (d) – the variations in the GAE trend component for the 160 Hz channel. According to [Gavrilov and Buss, 2015].
Citation: Gavrilov V. A., A. V. Naumov (2017), Modulation of geoacoustic emission intensity by time-varying electric field, Russ. J. Earth Sci., 17, ES1003, doi:10.2205/2017ES000591.
Copyright 2017 by the Geophysical Center RAS.
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