Abstract

The hypothesis that large earthquakes in the Baikal region are a response to bifurcations in nonlinear resonance hysteresis in a system consisting of three oscillators, attractor structures of riftogenesis, is substantiated. The hypothesis is confirmed by the spatial-temporal and magnitude distribution of large earthquakes: all the pairs of earthquakes with magnitude MLH > 5.5 that took place in the region within a small time period but were remote from one another show fair agreement with the main theoretical conclusions.

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