Add to ORKGThe seismic moment of the 1979 Imperial Valley earthquake is determined to be 6 x 10^(18) N·m (that is, M_w=6.5) from long-period Love and Rayleigh waves. The ratio of local magnitude M_L, to M_W for the event is 1.02, significantly larger than the value 0.90 for the 1940 Imperial Valley earthquake
Teleseismic, long-period P-waveforms are modeled to obtain estimates of the source parameters for t...
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 seismic moment of the 1979 Imperial Valley earthquake is determined to be 6 x 10^(18) N·m (that...
Long-period surface waves recorded on the north-south Pasadena strainmeter are used to determine the...
The mechanism of the May 2, 1983, Coalinga, California earthquake determined from long-period surfac...
The mechanism of the May 2, 1983, Coalinga, California earthquake determined from long-period surfac...
Observations of Love and Rayleigh waves on WWSSN and Canadian Network seismograms have been used to ...
Observations of Love and Rayleigh waves on WWSSN and Canadian Network seismograms have been used to ...
The seismic moment and source orientation of the 8 November 1980 Eureka, California, earthquake (M_s...
The seismic moment and source orientation of the 8 November 1980 Eureka, California, earthquake (M_s...
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 prominent long-period wave with a duration of 2000 sec or longer was recorded with a very-broadban...
A prominent long-period wave with a duration of 2000 sec or longer was recorded with a very-broadban...
Teleseismic, long-period P-waveforms are modeled to obtain estimates of the source parameters for t...
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 seismic moment of the 1979 Imperial Valley earthquake is determined to be 6 x 10^(18) N·m (that...
Long-period surface waves recorded on the north-south Pasadena strainmeter are used to determine the...
The mechanism of the May 2, 1983, Coalinga, California earthquake determined from long-period surfac...
The mechanism of the May 2, 1983, Coalinga, California earthquake determined from long-period surfac...
Observations of Love and Rayleigh waves on WWSSN and Canadian Network seismograms have been used to ...
Observations of Love and Rayleigh waves on WWSSN and Canadian Network seismograms have been used to ...
The seismic moment and source orientation of the 8 November 1980 Eureka, California, earthquake (M_s...
The seismic moment and source orientation of the 8 November 1980 Eureka, California, earthquake (M_s...
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 prominent long-period wave with a duration of 2000 sec or longer was recorded with a very-broadban...
A prominent long-period wave with a duration of 2000 sec or longer was recorded with a very-broadban...
Teleseismic, long-period P-waveforms are modeled to obtain estimates of the source parameters for t...
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...