Influence of the Shape of a Nonisometric Mountain Relief on the Characteristics of Seismic Oscillations
摘要
Abstract
Instrumental seismological observations were used to study the features of horizontal oscillation amplitudes along and across the crest of a mountain range during earthquakes. It is shown that the spectral amplitudes of oscillations in the direction across the ridge significantly exceed the amplitudes of oscillations along the ridge in a wide frequency range, regardless of the azimuth to the epicenter, and the frequencies of natural oscillations along and across the ridge also differ significantly.