Exploiting seismic signal and noise in an intracratonic environment to constrain crustal structure and source parameters of infrequent earthquakes
In many regions of the world characterized by a relatively low rate of seismicity, the determination of local and regional seismic source parameters is often restricted to an analysis of the first onsets of P waves (or first motion analysis) due to incomplete information about Earth structure and the small size of the events. When rare large earthquakes occur in these regions, their waveforms can be used to model Earth structure. This, however, makes the nature of the earthquake source...[Show more]
|Collections||ANU Research Publications|
|Source:||Geophysical Journal International|
|01_Young_Exploiting_seismic_signal_and_2012.pdf||5.72 MB||Adobe PDF|
|02_Young_Exploiting_seismic_signal_and_2012.pdf||5.72 MB||Adobe PDF|
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