RUSSIAN JOURNAL OF EARTH SCIENCES, VOL. 15, ES4003, doi:10.2205/2015ES000557, 2015
Figure 3. The results of the in situ experiment in the G-1 borehole for a depth of 1012 m: (a) the variations in the amplitude of diurnal variations and the trend of the GAE; (b) the diurnal variations of the external EMR in the frequency band of $160 \pm 20$ Hz.
Citation: Panteleev I. A., V. A. Gavrilov (2015), Implications of electrokinetic processes for the intensity of geoacoustic emission in the time vicinity of a tectonic earthquake: A theoretical study, Russ. J. Earth Sci., 15, ES4003, doi:10.2205/2015ES000557.
Copyright 2015 by the Geophysical Center RAS.
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