Add to ORKGThe seismic signatures of isolated body phases from many deep-focus earthquakes were analyzed in the time domain. Most shocks were found to be multiple events when examined in detail. The time history derived from P waves for single events predict synthetic S-wave shapes that match the observations, indicating compatibility with shear dislocation theory. Several other features of source functions in the time domain have been brought to light
With a generalized inverse technique, WWSSN (World-Wide Standard Seismograph Network) long-period P ...
In the past few years, our understanding of earth structure and of earthquakes has increased dramati...
Source parameters of two shallow earthquakes have been determined by the time-domain analysis of sho...
The seismic signatures of isolated body phases from many deep-focus earthquakes were analyzed in the...
Broad-band recordings of aftershocks of the Pt. Mugu earthquake at small epicentral distances provid...
Broadband vertical P-wave records are analyzed from 63 of the largest shallow subduction zone earthq...
Broadband vertical P-wave records are analyzed from 63 of the largest shallow subduction zone earthq...
A procedure for modeling P and PL waves recorded on long-period WWSSN instruments at ranges 1° to 12...
The dynamical processes at the source of eleven deep-focus and intermediate-depth earthquakes that o...
Deconvolution of seismic data is an important component of signal processing that aims to remove the...
Modern broadband seismic instrumentation has provided enormous opportunities to retrieve the informa...
We developed a new method to determine earthquake source time functions and focal depths. It uses th...
With a generalized inverse technique, WWSSN (World-Wide Standard Seismograph Network) long-period P ...
In the following pages are presented certain rapid and convenient methods for interpreting the recor...
In the following pages are presented certain rapid and convenient methods for interpreting the recor...
With a generalized inverse technique, WWSSN (World-Wide Standard Seismograph Network) long-period P ...
In the past few years, our understanding of earth structure and of earthquakes has increased dramati...
Source parameters of two shallow earthquakes have been determined by the time-domain analysis of sho...
The seismic signatures of isolated body phases from many deep-focus earthquakes were analyzed in the...
Broad-band recordings of aftershocks of the Pt. Mugu earthquake at small epicentral distances provid...
Broadband vertical P-wave records are analyzed from 63 of the largest shallow subduction zone earthq...
Broadband vertical P-wave records are analyzed from 63 of the largest shallow subduction zone earthq...
A procedure for modeling P and PL waves recorded on long-period WWSSN instruments at ranges 1° to 12...
The dynamical processes at the source of eleven deep-focus and intermediate-depth earthquakes that o...
Deconvolution of seismic data is an important component of signal processing that aims to remove the...
Modern broadband seismic instrumentation has provided enormous opportunities to retrieve the informa...
We developed a new method to determine earthquake source time functions and focal depths. It uses th...
With a generalized inverse technique, WWSSN (World-Wide Standard Seismograph Network) long-period P ...
In the following pages are presented certain rapid and convenient methods for interpreting the recor...
In the following pages are presented certain rapid and convenient methods for interpreting the recor...
With a generalized inverse technique, WWSSN (World-Wide Standard Seismograph Network) long-period P ...
In the past few years, our understanding of earth structure and of earthquakes has increased dramati...
Source parameters of two shallow earthquakes have been determined by the time-domain analysis of sho...