1998
DOI: 10.21236/ada376570
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Study of Low and Lg from Explosions and Its Application to Seismic Monitoring of the CTBT

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Cited by 2 publications
(2 citation statements)
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“…
Rg scattering has often been suggested as the source of the regional Lg phase generated by explosions (e.g., Patton and Taylor, 1995;Gupta and Wagner, 1998). The main point of our paper (Stevens et al, 2009) was that it is very difficult to get enough energy out of Rg to generate the observed Lg and that direct generation of S by the source or pS conversion are likely to be stronger sources of Lg than Rg scattering.
…”
mentioning
confidence: 70%
“…
Rg scattering has often been suggested as the source of the regional Lg phase generated by explosions (e.g., Patton and Taylor, 1995;Gupta and Wagner, 1998). The main point of our paper (Stevens et al, 2009) was that it is very difficult to get enough energy out of Rg to generate the observed Lg and that direct generation of S by the source or pS conversion are likely to be stronger sources of Lg than Rg scattering.
…”
mentioning
confidence: 70%
“…This has been interpreted as evidence of Rg scattering (e.g. Gupta and Wagner, 1998) because Rg also falls off rapidly with frequency. Goldstein (1995) however provides an alternate explanation.…”
Section: Lg Spectral Slopesmentioning
confidence: 96%