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The results of regular instrumental observations over geomagnetic field variations in the zones of influence of tectonic faults
during movement of seismic waves of varied intensity are presented. It has been shown that seismic waves with an amplitude
more than 5–10 μm/s, traveling across the fault zone, always produced geomagnetic field variations. At weaker seismic disturbances,
geomagnetic field variations are of the “glimmer” character, and the relative frequency of appearance of the effect drops
as the seismic wave amplitude decreases. The quantitative dependence between the maximal value of the full vector of variations
in geomagnetic field induction in a fault zone and the amplitude of the seismic disturbance has been found for the first time. 相似文献
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