Reducing Systematic Errors for Seismic Event Locations Using a Model Incorporating Anisotropic Regional Structures
Abstract
We have utilized a mapping of the lateral and anisotropic variations in Pn velocities beneath continents across the globe (Smith & Ekstrom, 1999) to predict travel times of P-wave propagation at distances of 2 - 14 degrees. At such distances, the phase Pn is in the seismic phase that is most frequently reported and that thus controls the location accuracy. This is important in CTBT applications as many events of interest are only detected at these distances. We have thus worked on reducing the systematic errors in Pn travel-times and the resulting seismic event location at regional distances using our mapping.
Document Details
- Document Type
- Technical Report
- Publication Date
- Mar 01, 2006
- Accession Number
- ADA456301
Entities
People
- Douglas A. Wiens
- Gideon P. Smith
Organizations
- Washington University in St. Louis