The well-known first motion method of Nakano and Byerly is extended, generalized and combined with recent new ideas in body wave theory in order to set up a routine procedure for extracting source parameters from spectral analysis of isolated P and S pulses recorded at a net of standardized stations around a non-shallow source. The method consists of compensating the observed spectrums for instrumental and propagational effects. A combined study of the resulting radiation patterns, initial phases, and the initial amplitudes will render information regarding the spatial and temporal nature of deep and intermediate earthquake sources as seen through the spectral window of 10-100 seconds. The shorter periods can be used for source studies o...
Expressions for displacements on the surface of a layered half space due to an arbitrary oriented sh...
In the past few years, our understanding of earth structure and of earthquakes has increased dramati...
The generalized linear inverse technique has been adapted to the problem of determining an earthquak...
The well-known first motion method of Nakano and Byerly is extended, generalized and combined with r...
The present work concerns a study on the radiation and propagation of seismic body waves. Based on ...
Since 1960, new methods have been developed for extracting source information from surface-wave sig...
With a generalized inverse technique, WWSSN (World-Wide Standard Seismograph Network) long-period P ...
With a generalized inverse technique, WWSSN (World-Wide Standard Seismograph Network) long-period P ...
Fourier analysis of mantle Love and Rayleigh waves from the source of the Kamchatka earthquake of No...
Fourier analysis of mantle Love and Rayleigh waves from the source of the Kamchatka earthquake of No...
The Pasadena seismograms of the Mongolian earthquake of December 4, 1957, were studied. Mantle Rayle...
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 composite compute program has been devised for a fast reduction of multistation seismic data in th...
In the past few years, our understanding of earth structure and of earthquakes has increased dramati...
Expressions for displacements on the surface of a layered half space due to an arbitrary oriented sh...
In the past few years, our understanding of earth structure and of earthquakes has increased dramati...
The generalized linear inverse technique has been adapted to the problem of determining an earthquak...
The well-known first motion method of Nakano and Byerly is extended, generalized and combined with r...
The present work concerns a study on the radiation and propagation of seismic body waves. Based on ...
Since 1960, new methods have been developed for extracting source information from surface-wave sig...
With a generalized inverse technique, WWSSN (World-Wide Standard Seismograph Network) long-period P ...
With a generalized inverse technique, WWSSN (World-Wide Standard Seismograph Network) long-period P ...
Fourier analysis of mantle Love and Rayleigh waves from the source of the Kamchatka earthquake of No...
Fourier analysis of mantle Love and Rayleigh waves from the source of the Kamchatka earthquake of No...
The Pasadena seismograms of the Mongolian earthquake of December 4, 1957, were studied. Mantle Rayle...
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 composite compute program has been devised for a fast reduction of multistation seismic data in th...
In the past few years, our understanding of earth structure and of earthquakes has increased dramati...
Expressions for displacements on the surface of a layered half space due to an arbitrary oriented sh...
In the past few years, our understanding of earth structure and of earthquakes has increased dramati...
The generalized linear inverse technique has been adapted to the problem of determining an earthquak...