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We suggest a method of fitting of a zero-range model of a tectonic plateunder a boundary stress on the basis of comparison of the theoretical formulaefor the corresponding eigenfunctions/eigenvalues with the results extractionunder monitoring, in the remote zone, of non-random (regular) oscillations ofthe Earth with periods 0.2-6 hours, on the background seismic process, in caseof low seismic activity. Observations of changes of the characteristics of theoscillations (frequency, amplitude and polarization) in course of time,together with the theoretical analysis of the fitted model, would enable us tolocalize the stressed zone on the boundary of the plate and estimate the riskof a powerful earthquake at the zone.

Tectonic plate under a localized boundary stress: fitting of a zero-range solvable model