The models of Moho depth, crustal Vp/Vs ratio, depth of sedimentary velocity discontinuity, and sedimentary Vp/Vs ratio in the Permian Basin region were derived from P receiver functions.
|Title||Seismic Features of the Permian Basin Region from Receiver Function Analysis|
|Type||Moho depth, crustal Vp/Vs ratio, depth of sedimentary velocity discontinuity, and sedimentary Vp/Vs ratio|
|Short Description||The models of Moho depth, crustal Vp/Vs ratio, depth of sedimentary velocity discontinuity, and sedimentary Vp/Vs ratio in the Permian Basin region were derived from P receiver functions.
|Bureau of Economic Geology, Jackson School of Geosciences|
|The University of Texas at Austin|
|10100 Burnet Road, Austin, TX, 78758, USA|
|Model Download||Moho_Depth_Error.nc (see metadata), is the netCDF Moho depth model expressed as depth in km
Crust_VpVs_ratio_Error.nc (see metadata), is the netCDF of the crustal Vp/Vs ratio
Sedimentary_Velocity_Discontinuity_Depth_Error.nc (see metadata), is the netCDF file of the Sedimentary velocity discontinuity depth model expressed as depth in km
Sedimentary_VpVs_Ratio_Error.nc (see metadata), is the netCDF of Sedimentary Vp/Vs ratio
|Original Model Repository|
|Area||Permian Basin region (latitude: 30.0°/33.0°; longitude: -105.0°/-102.2°)|
|Data Set Description||The models include: 1) Moho depth values. 2) Crustal Vp/Vs ratio values. 3) Sedimentary velocity discontinuity depth values. And 4) Sedimentary Vp/Vs ratio. We obtained 3120 receiver functions in the Permian Basin region, and then applied waveform fitting method to derive the depth and Vp/Vs ratio models. The sedimentary velocity discontinuity refers to the first-order velocity discontinuity in sediment basin, above the basin basement. Sea level is zero depth.|
Citations and DOIs
To cite the original work behind this Earth model:
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:
Model provided by Peng Li