RUSSIAN JOURNAL OF EARTH SCIENCES, VOL. 14, ES2003, doi:10.2205/2014ES000541, 2014


Figure 7. The example of short realizations of simultaneous time series of GAE ($Z$-channel, depth 1012 m) and EMI in the G-1 borehole: (a) the GAE signal in the 1000 Hz band; (b) the GAE signal at a frequency of 150 Hz; (c) the EMI signal at a frequency of 150 Hz.


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Citation: Gavrilov V. A. (2014), On the mechanism of intensity variations of geoacoustic emission caused under the action of audio-frequency electromagnetic field, Russ. J. Earth Sci., 14, ES2003, doi:10.2205/2014ES000541.


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