Abstract
The location procedures of seismic events are influenced by two major classes of errors, the error in picking individual seismic phases and modeling error due to the departure of the real Earth from the reference model used in the location. The role of picking errors can be assessed by a nonlinear analysis using a Monte Carlo procedure. The modeling error due to the influence of lateral heterogeneity in the Earth is examined by comparing the locations of the same event using different combinations of phases and network geometries. By relocating events with network geometries corresponding to the different magnitudes, it is found that the location of the event can be affected significantly by the magnitude, and when using robust statistics to describe earthquake residuals, the mislocation can occur in a systematic manner. The effect is marked in regions with significant lateral variations in seismic velocities. -from Authors
Original language | English |
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Pages (from-to) | 1978-1990 |
Number of pages | 13 |
Journal | Bulletin - Seismological Society of America |
Volume | 84 |
Issue number | 6 |
Publication status | Published - 1994 |