Add to ORKGStatistical characteristics of the P wave travel time residuals have been studied by using the aftershocks of the 1965 Rat Islands, Aleutian Earthquake. There are not a few stations of which mean residuals are as large as several seconds. It will be necessary to adopt "station corrections" in order to get more precise locations of hypocenters. Variances for residuals noted with eP and P onsets are larger than the ones for iP onsets or total observations. Generally the mean values are 0.0, and the standard deviation are 1.1 seconds
The 9 March 1957 Aleutian earthquake has been estimated as the third largest earthquake this century...
The 9 March 1957 Aleutian earthquake has been estimated as the third largest earthquake this century...
Computing the magnitude of an earthquake requires correcting for the propagation effects from the so...
Statistical characteristics of the P wave travel time residuals have been studied by using the after...
Abstract P-wave velocity variations may provide precursory information before large earthquakes. We ...
Teleseismic arrivals at 30 stations in the vicinity of Hollister, California, have been analyzed for...
The regional variation of the P-wave travel time residual is investigated. USCGS and Soviet data are...
P-wave travel time residuals from JB curves, in the distance range from 0° to 40°, along the Aleutia...
The regional variation of the P-wave travel time residual is investigated. USCGS and Soviet data are...
P-wave delays at Tinemaha, China Lake, Pasadena, Riverside, Hayfield and Barrett, stations of the CI...
The great Rat Islands underthrusting earthquake (Mw = 8.7), of February 4, 1965, represents subducti...
Teleseismic P residuals have been monitored as a function of time at 13 stations in southern Califor...
Teleseismic P residuals have been monitored as a function of time at 13 stations in southern Califor...
P-wave travel time residuals from JB curves, in the distance range from 0° to 40°, along the Aleutia...
Approximately 3300 shallow focus earthquakes and 1000 seismic stations have been used in a study of ...
The 9 March 1957 Aleutian earthquake has been estimated as the third largest earthquake this century...
The 9 March 1957 Aleutian earthquake has been estimated as the third largest earthquake this century...
Computing the magnitude of an earthquake requires correcting for the propagation effects from the so...
Statistical characteristics of the P wave travel time residuals have been studied by using the after...
Abstract P-wave velocity variations may provide precursory information before large earthquakes. We ...
Teleseismic arrivals at 30 stations in the vicinity of Hollister, California, have been analyzed for...
The regional variation of the P-wave travel time residual is investigated. USCGS and Soviet data are...
P-wave travel time residuals from JB curves, in the distance range from 0° to 40°, along the Aleutia...
The regional variation of the P-wave travel time residual is investigated. USCGS and Soviet data are...
P-wave delays at Tinemaha, China Lake, Pasadena, Riverside, Hayfield and Barrett, stations of the CI...
The great Rat Islands underthrusting earthquake (Mw = 8.7), of February 4, 1965, represents subducti...
Teleseismic P residuals have been monitored as a function of time at 13 stations in southern Califor...
Teleseismic P residuals have been monitored as a function of time at 13 stations in southern Califor...
P-wave travel time residuals from JB curves, in the distance range from 0° to 40°, along the Aleutia...
Approximately 3300 shallow focus earthquakes and 1000 seismic stations have been used in a study of ...
The 9 March 1957 Aleutian earthquake has been estimated as the third largest earthquake this century...
The 9 March 1957 Aleutian earthquake has been estimated as the third largest earthquake this century...
Computing the magnitude of an earthquake requires correcting for the propagation effects from the so...