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Next: SHEARER's EARTHQUAKE STACKS Up: Claerbout: Earthquake stacks Previous: Claerbout: Earthquake stacks


The figures in this paper show Professor Peter Shearer's stacks over many earthquakes at constant epicentral distance (offset angle). Notice that the time scale is minutes and the offset is degrees of angle on the earth's surface. Otherwise, there are remarkable similarities to conventional exploration seismic data. For details of how the stacks were made, see the references.

Stanford Exploration Project