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The ability to confidently estimate the depths of small-to-medium sized (3.5≤ mb≤ 5.5) seismic disturbances is important both in plate tectonics studies, and when monitoring compliance with the Comprehensive Nuclear-Test-Ban Treaty (CTBT). Seismic source depths can be determined by identification of the teleseismic depth phases pP and sP, and also by modelling surface wave amplitude spectra. The...

Estimating earthquake source depths by combining surface wave amplitude spectra and teleseismic depth phase observations