Summary
DNA10-S model, Obrebski, Allen, Pollitz & Hung (2011), integrates teleseismic body-wave traveltime and surface-wave phase velocity measurements into a single inversion to constrain the S-wave velocity structure beneath the western US.
Quicklinks
Description
Name | DNA10-S |
Title | S-velocity model for the western US integrating body- and surface-wave constraints |
Type | 3-D Tomography Earth Model |
Sub Type | S velocity perturbation (%) |
Year | 2010 |
Short Description | The DNA10-S model integrates teleseismic body-wave traveltime and surface-wave phase velocity measurements into a single inversion to constrain the S-wave velocity structure beneath the western US (from the Pacific coast to ~100° W, from Mexico to Canada). |
Authors: | |
Mathias Obrebski | |
Department of Earth and Planetary Science | |
University of California, Berkeley | |
California, USA | |
Richard M. Allen | |
Department of Earth and Planetary Science | |
University of California, Berkeley | |
California, USA | |
Fred Pollitz | |
US Geological Survey | |
Menlo Park, CA, USA | |
Shu-Huei Hung | |
Department of Geosciences | |
National Taiwan University | |
Taipei, Taiwan | |
Previous Model | |
Reference Model | N/A |
Model Download | |
original model files from the model download page | |
DNA10-S_percent.nc (see metadata ), is the netCDF file for the model | |
Model Homepage | http://seismo.berkeley.edu/~rallen/research/dna/dna10 |
Depth Coverage | 0 to 1000 km |
Area | Northwestern United States (30°/50°, -126°/-98°) |
Data Set Description | [ Obrebski et al. (2011)] he station distribution that used in this study covers all the major magmato-tectonic features of the active western United States plus the westernmost part of the stable cratonic United States. This includes more than 1200 stations from the USArray transportable array, regional seismic networks, and temporary seismic deployments. Data were recorded from 2006 January to 2010 January. Relative traveltimes of teleseismic body waves (S and SKS) obtained from about 162 earthquakes, and surface wave phase velocity measurements from 167 eartqhuakes were used to constrain the model. |
Citations and DOIs
To cite the original work behind this Earth model:
- Obrebski, M., R.M. Allen, F. Pollitz, and S.-H. Hung. 2011. “Lithosphere-asthenosphere interaction beneath the western United States from the joint inversion of body-wave traveltimes and surface-wave phase velocities.” Geophys. J. Int. 185:1003-1021. https://doi.org/10.1111/j.1365-246X.2011.04990.x.
To cite IRIS DMC Data Products effort:
- Trabant, C., A. R. Hutko, M. Bahavar, R. Karstens, T. Ahern, and R. Aster (2012), Data Products at the IRIS DMC: Stepping Stones for Research and Other Applications, Seismological Research Letters, 83(5), 846–854, https://doi.org/10.1785/0220120032.
DOI for this EMC webpage:
Credits
Model provided by Richard M. Allen
Timeline
- 2011-10-03
- Online