Identification of hydrogeochemical and hydrodynamic effects with manifestations of seismicity in the territory of Kyrgyzstan
For the first time, the data of the spatial and temporal restructuring of the parameters of thermal mineral waters (TMW) of Kyrgyzstan, associated with the periods before, during and after the strong earthquakes that occurred in 1970-2015, were generalized. reliable separation of the useful signal from «regular» interference. It is shown that hydroanomalies lasting from the first hours and days to several months, in terms of shapes and contrast, without repeating from one earthquake to another, arise during seismic events at K ≥11.