Abstract
The article is devoted to the study of the influence of watering of the rock environment on post-seismic activity in the deposits of the Khibiny mountains. Initial data are the results of long-term monitoring of seismicity and observations of water inflows. At a qualitative level, the influence of watering of the environment on the b-value of the Gutenberg – Richter distribution of magnitudes of triggered events, as well as on the parameters of the Omori – Utsu law, which describes the post-seismic activity decay rate over time, was studied.
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