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Research Article|
May 01, 1998
Comparing Shear-Wave Velocity Profiles From Inversion of Surface-Wave Phase Velocities with Downhole Measurements: Systematic Differences Between the CXW Method and Downhole Measurements at Six USC Strong-Motion Sites
David M. Boore
;
David M. Boore
U.S. Geological Survey
345 Middlefield Road
Menlo Park, CA 94025
dboore@isdmnl.wr.usgs.gov
leotb@mail.utexas.edu
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Leo T. Brown
Leo T. Brown
U.S. Geological Survey
345 Middlefield Road
Menlo Park, CA 94025
dboore@isdmnl.wr.usgs.gov
leotb@mail.utexas.edu
Search for other works by this author on:
Seismological Research Letters (1998) 69 (3): 222-229.
Article history
first online:
09 Mar 2017
Citation
David M. Boore, Leo T. Brown; Comparing Shear-Wave Velocity Profiles From Inversion of Surface-Wave Phase Velocities with Downhole Measurements: Systematic Differences Between the CXW Method and Downhole Measurements at Six USC Strong-Motion Sites. Seismological Research Letters ; 69 (3): 222–229. doi: https://doi.org/10.1785/gssrl.69.3.222
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Index Terms/Descriptors
- body waves
- downhole methods
- earthquakes
- elastic waves
- equations
- frequency
- geophysical methods
- geophysical profiles
- ground motion
- guided waves
- Landers earthquake 1992
- methods
- Northridge earthquake 1994
- S-waves
- seismic methods
- seismic profiles
- seismic waves
- seismicity
- seismograms
- strong motion
- surface waves
- traveltime
- velocity
- wave amplification