Dorris M. Hankins
Abstract
abstract Comparison of gnome seismic signals at four stations with seismograms from an explosion in tuff show relatively more energy in the Pg phase than would be predicted from first phase amplitudes. Dispression curve for a surface layer Rayleigh mode is given.
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abstract Comparison of gnome seismic signals at four stations with seismograms from an explosion in tuff show relatively more energy in the Pg phase than would be predicted from first phase amplitudes. Dispression curve for a surface layer Rayleigh mode is given.
Key concepts: Seismogram, Geology, Seismology, Amplitude, Seismic energy, Rayleigh wave, Phase (matter), Mode (computer interface)