A composite compute program has been devised for a fast reduction of multistation seismic data in the period range 50–500 sec for mantle surface waves and 20–100 sec for body waves. The analysis aims at the reconstruction of the seismic source from the spectrum of its far radiation field and the correlation of its parameters with its depth, size and regional environment. The capability of the computational procedure has been demonstrated in two studies of WWNSS records: one includes a spectral analysis of surface waves from a shallow shock in the Kurile Islands; the other includes a spectral analysis of P waves from 9 shocks in the depth range 550–700 km at Fiji, Mariana, Java, Japan, Peru and Brazil. Other applications of the prop...
Source-mechanism is derived from amplitude and phase spectra of mantle Love and Rayleigh waves of th...
Source-mechanism is derived from amplitude and phase spectra of mantle Love and Rayleigh waves of th...
A seismic analyzing system of analogue type is constructed for the study of teleseismic signals whic...
The depths and source mechanisms of nine large shallow earthquakes were determined from long-period ...
The depths and source mechanisms of nine large shallow earthquakes were determined from long-period ...
In general, the depths of shallow earthquakes are poorly resolved in current catalogues. Variations ...
In general, the depths of shallow earthquakes are poorly resolved in current catalogues. Variations ...
The depths and source mechanisms of nine large shallow earthquakes were determined from long-period ...
In this thesis, a method to retrieve the source finiteness, depth of faulting, and the mechanisms of...
The well-known first motion method of Nakano and Byerly is extended, generalized and combined with r...
The well-known first motion method of Nakano and Byerly is extended, generalized and combined with r...
The Pasadena seismograms of the Mongolian earthquake of December 4, 1957, were studied. Mantle Rayle...
Normal mode solutions for a spherical earth model are superposed to obtain realistic synthetic surfa...
Since 1960, new methods have been developed for extracting source information from surface-wave sig...
Normal mode solutions for a spherical earth model are superposed to obtain realistic synthetic surfa...
Source-mechanism is derived from amplitude and phase spectra of mantle Love and Rayleigh waves of th...
Source-mechanism is derived from amplitude and phase spectra of mantle Love and Rayleigh waves of th...
A seismic analyzing system of analogue type is constructed for the study of teleseismic signals whic...
The depths and source mechanisms of nine large shallow earthquakes were determined from long-period ...
The depths and source mechanisms of nine large shallow earthquakes were determined from long-period ...
In general, the depths of shallow earthquakes are poorly resolved in current catalogues. Variations ...
In general, the depths of shallow earthquakes are poorly resolved in current catalogues. Variations ...
The depths and source mechanisms of nine large shallow earthquakes were determined from long-period ...
In this thesis, a method to retrieve the source finiteness, depth of faulting, and the mechanisms of...
The well-known first motion method of Nakano and Byerly is extended, generalized and combined with r...
The well-known first motion method of Nakano and Byerly is extended, generalized and combined with r...
The Pasadena seismograms of the Mongolian earthquake of December 4, 1957, were studied. Mantle Rayle...
Normal mode solutions for a spherical earth model are superposed to obtain realistic synthetic surfa...
Since 1960, new methods have been developed for extracting source information from surface-wave sig...
Normal mode solutions for a spherical earth model are superposed to obtain realistic synthetic surfa...
Source-mechanism is derived from amplitude and phase spectra of mantle Love and Rayleigh waves of th...
Source-mechanism is derived from amplitude and phase spectra of mantle Love and Rayleigh waves of th...
A seismic analyzing system of analogue type is constructed for the study of teleseismic signals whic...