Relative excitation of surface waves by earthquakes and underground explosions

Liebermann, Robert C.; Pomeroy, Paul W.

doi:10.1029/jb074i006p01575

“…Past studies (e.g., Liebermann and Pomeroy, 1969, -89-1973) as well as this analysis, suggested that discrimination on a regional basis will be more successful than when all events are treated together.…”

Section: Discrimination Of Earthquakes and Explosions On A Regional Bmentioning

confidence: 99%

Analysis of Selected Seismic Events from Asia in a Seismic Discrimination Context

Sobel¹,

Seggern²

1978

3

0

View full text Add to dashboard Cite

“…In analyzing m D :M s data, Liebermann and Pomeroy (1969) and Basham (1969) noted that the i»tj :M s data for explosions and earthquakes in the western United States are anomalous with respect to such data for the Aleutians, Algeria, and the USSR. Marshall and Basham (1972) confirmed that the m^Mg relations for explosions in the western US differ from those for explosions in the Aleutians, the USSR, and China, but they did not detect any regional differences in litf^ data for earthquakes.…”

Section: Body Vs Surface-wave Magnitude Relations For Underground Nucmentioning

confidence: 99%

Inelastic processes in seismic wave generation by underground explosions

Rodean¹

1980

1

0

View full text Add to dashboard Cite

There are similarities and differences between chemical and nuclear explosions underground. Host of the differences are in the early stages of the explosions. The later stages are similar with respect to seismic wave generation. Three sources of seismic waves from explosions are coincident in space and time, or nearly so: the explosion itself, explosion-induced tectonic strain release, and (probably) spall-closure following explosion-produced spall. Cavity collapse and explosion-induced aftershocks are two sources of delayed seismic signals. Theories, computer calcula tions, and measurements of spherical stress waves from explosions are described and compared, with emphasis on the transition from inelastic to almost-elastic relations between stress and strain. Two aspects of nonspherical explosion geometry are considered: tectonic strain release and surface spall. Tectonic strain release affects the generation of surface waves; spall closure may also. The forward problem in seismology can, in principle, be solved by calculations beginning with explosive detonation and ending with the synthetic seismogram. The inverse problem can also, in principle, be solved by inverting observed seismic data to obtain an "equivalent elastic source," but the solution cannot extend backward in space and time into the nonlinear inelastic processes of the explosion. The reduced-displacement potential is a common solution (the "equivalent elastic source") of the forward and inverse problems, assuming a spherical source. Measured reduceddisplacement potentials are compared with potentials calculated as solutions of the direct and inverse problems; there are signifi cant differences between the results of the two types of calcula tions and between calculations and measurements. The simple

show abstract

“…In analyzing m D :M s data, Liebermann and Pomeroy (1969) and Basham (1969) explosions and earthquakes in the western United States are anomalous with respect to such data for the Aleutians, Algeria, and the USSR. Marshall and Basham (1972) confirmed that the m^Mg relations for explosions in the western US differ from those for explosions in the Aleutians, the USSR, and China, but they did not detect any regional differences in litf^ data for earthquakes.…”

Section: Body Vs Surface-wave Magnitude Relations For Underground Nucmentioning

confidence: 99%

Inelastic Processes in Seismic Wave Generation by Underground Explosions

Rodean

¹

1981

Identification of Seismic Sources — Earthquake or Underground Explosion

View full text Add to dashboard Cite

There are similarities and differences between chemical and nuclear explosions underground. Host of the differences are in the early stages of the explosions. The later stages are similar with respect to seismic wave generation. Three sources of seismic waves from explosions are coincident in space and time, or nearly so: the explosion itself, explosion-induced tectonic strain release, and (probably) spall-closure following explosion-produced spall. Cavity collapse and explosion-induced aftershocks are two sources of delayed seismic signals. Theories, computer calcula tions, and measurements of spherical stress waves from explosions are described and compared, with emphasis on the transition from inelastic to almost-elastic relations between stress and strain. Two aspects of nonspherical explosion geometry are considered: tectonic strain release and surface spall. Tectonic strain release affects the generation of surface waves; spall closure may also. The forward problem in seismology can, in principle, be solved by calculations beginning with explosive detonation and ending with the synthetic seismogram. The inverse problem can also, in principle, be solved by inverting observed seismic data to obtain an "equivalent elastic source," but the solution cannot extend backward in space and time into the nonlinear inelastic processes of the explosion. The reduced-displacement potential is a common solution (the "equivalent elastic source") of the forward and inverse problems, assuming a spherical source. Measured reduceddisplacement potentials are compared with potentials calculated as solutions of the direct and inverse problems; there are signifi cant differences between the results of the two types of calcula tions and between calculations and measurements. The simple

show abstract

Relative excitation of surface waves by earthquakes and underground explosions

Cited by 74 publications

References 38 publications

Analysis of Selected Seismic Events from Asia in a Seismic Discrimination Context

Analysis of Selected Seismic Events from Asia in a Seismic Discrimination Context

Inelastic processes in seismic wave generation by underground explosions

Inelastic Processes in Seismic Wave Generation by Underground Explosions

Contact Info

Product

Resources

About