RUSSIAN JOURNAL OF EARTH SCIENCES, VOL. 13, ES1002, doi:10.2205/2013ES000527, 2013

Figure 3. Degradation of GAE response compared to seismic activity. 1 – presence of detected GAE response, 2 – data omissions. Arrows point at earthquakes of $M_{LH} \geq 5.0$ in the zone of $R \leq 300$ km and $M_{LH} \geq 5.5$ in the zone of $R \leq 550$ km. Earthquake of $M_w=7.3$ occurred at epicenter distance of about 1000 km at a depth of 459 km. Data on seismicity correspond to the "Catalog of earthquakes of the Kamchatka Branch of the Geophysical Survey of RAS". See the text.

 
Citation: Gavrilov V. A., I. A. Panteleev, G. V. Ryabinin, Yu. V. Morozova (2013), Modulating impact of electromagnetic radiation on geoacoustic emission of rocks, Russ. J. Earth Sci., 13, ES1002, doi:10.2205/2013ES000527.
 

Copyright 2013 by the Geophysical Center RAS.

Generated from LaTeX source by SemTeXML, v.1.2) software package.