Summary
Africa.ANT.Emry-etal.2018 is a 3-D isotropic shear-wave tomographic model of Africa and neighboring regions.
Quicklinks
Description
Name | Africa.ANT.Emry-etal.2018 |
Title | 3-D isotropic shear-wave model for Africa from full-wave ambient noise tomography |
Type | 3-D Tomography Earth Model |
Sub Type | Shear-wave velocity (km/s) |
Year | 2018 |
Short Description | Africa.ANT.Emry-etal.2018 is a 3-D isotropic shear-wave tomographic model of Africa and neighboring regions. Model is constrained by long period (40-340 sec.) Rayleigh waves from empirical Green’s functions (EGF) extracted from cross-correlation between station pairs. Data are inverted using finite-difference full-waveform simulations to construct finite-frequency sensitivity kernels. Model is iteratively updated, and the contributed model provides results following the 9th iteration. Best model resolution is at depths of ~100-400 km. |
Authors: | |
Erica Emry | |
Earth and Environmental Sciences | |
New Mexico Tech | |
Socorro, NM, USA | |
Yang Shen | |
Graduate School of Oceanography | |
University of Rhode Island | |
Narragansett, RI, USA | |
Andrew Nyblade | |
Department of Geosciences | |
Pennsylvania State University | |
University Park, PA, USA | |
Ashton Flinders | |
United States Geological Survey | |
Menlo Park, CA, USA | |
Xueyang Bao | |
Graduate School of Oceanography | |
University of Rhode Island | |
Narragansett, RI, USA | |
Previous Model | None |
Reference Model | Starting model was CRUST1.0 (Laske et al., 2013) underlain by AK135 (Kennett et al., 1995); the final model is provided as absolute shear-wave velocity (km/s). |
Model Download | Africa.ANT.Emry-etal.2018_kmps.nc (see metadata ), is the netCDF file for the model |
Model Homepage | |
Depth Coverage | Included in the netCDF are depths from 33-614 km; best model resolution is at ~100-400 km. |
Area | Africa and parts of the Arabian Peninsula and Mediterranean (latitude: -41.4° to 51.6°, longitude: -32.6° to 66.4°). |
Data Set Description | Ambient noise data were collected from 851 seismic stations located throughout Africa, the Middle East, and Southern Europe, and station-station cross-correlation was used to retrieve empirical Green’s functions (EGFs). EGFs with Rayleigh wave signal-to-noise ratio (SNR) > 5 were for 414 stations at periods of 7-340 sec. Data with SNR > 5 at periods of 40-340 sec periods (from 186 seismic stations) were used to invert for this upper-mantle model. |
Model Resolution: | Model inversion blocks are 1°x1° in the horizontal direction. Inversion block size increases with model depth in the vertical direction, from 11-34 km spacing. The best resolution exists at upper mantle depths (~100-400 km) between 25°S to 45°N and 0 to 50° E. |
Citations and DOIs
To cite the original work behind this Earth model:
- Emry, E. L., Shen, Y., Nyblade, A. A., Flinders, A., & Bao, X. (2018). Upper mantle Earth structure in Africa from full-wave ambient noise tomography. Geochemistry, Geophysics, Geosystems,19. https://doi.org/10.1029/2018GC007804
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:
References
- Kennett B.L.N., E.R. Engdahl and R. Buland. 1995. “Constraints on seismic velocities in the earth from travel times” Geophys. J. Int. 122:108-124.
- Laske, G., Masters., G., Ma, Z. and Pasyanos, M., Update on CRUST1.0 – A 1-degree Global Model of Earth’s Crust, Geophys. Res. Abstracts, 15, Abstract EGU2013-2658, 2013.
Credits
Model provided by Erica Emry
Timeline
- 2019-01-09
- online