Long-period surface waves recorded on the north-south Pasadena strainmeter are used to determine the seismic moments and fault parameters of the 19 May 1940 Imperial Valley, California, the 16 December 1954 Dixie Valley and Fairview Peak, Nevada, and the 18 August 1959 Hebgen Lake, Montana, earthquakes. Synthetic strain seismograms are matched with the observed strainmeter seismograms. Source parameters from the strainmeter modeling are more consistent with source parameters estimated from geodetic and geologic information than parameters estimated from short-period (<15 sec) body wave data. Long-period surface wave moment estimates agree well with geodetic estimates of moment, but are 1.5 to 5 times greater than moments obtained from model...
The availability of high dynamic range very broad band seismic data in recent years has greatly incr...
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...
The seismic moment of the 1979 Imperial Valley earthquake is determined to be 6 x 10^(18) N·m (that...
The seismic moment of the 1979 Imperial Valley earthquake is determined to be 6 x 10^(18) N·m (that...
The source mechanism of earthquakes in the California‐Nevada region was studied using surface wave a...
The source mechanism of earthquakes in the California‐Nevada region was studied using surface wave a...
The source mechanism of earthquakes in the California-Nevada region was studied using surface wave a...
The ratio of short- to long-period amplitude is expressed in terms of apparent stress, rigidity time...
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 ratio of short- to long-period amplitude is expressed in terms of apparent stress, rigidity time...
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...
A procedure for modeling P and PL waves recorded on long-period WWSSN instruments at ranges 1° to 12...
The availability of high dynamic range very broad band seismic data in recent years has greatly incr...
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...
The seismic moment of the 1979 Imperial Valley earthquake is determined to be 6 x 10^(18) N·m (that...
The seismic moment of the 1979 Imperial Valley earthquake is determined to be 6 x 10^(18) N·m (that...
The source mechanism of earthquakes in the California‐Nevada region was studied using surface wave a...
The source mechanism of earthquakes in the California‐Nevada region was studied using surface wave a...
The source mechanism of earthquakes in the California-Nevada region was studied using surface wave a...
The ratio of short- to long-period amplitude is expressed in terms of apparent stress, rigidity time...
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 ratio of short- to long-period amplitude is expressed in terms of apparent stress, rigidity time...
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...
A procedure for modeling P and PL waves recorded on long-period WWSSN instruments at ranges 1° to 12...
The availability of high dynamic range very broad band seismic data in recent years has greatly incr...
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...