Rajaonarison, Tahiry A; Stamps, D Sarah; Fishwick, Stewart; Brune, Sascha; Glerum, Anne; Hu, Jiashun (2019): Synthetic Splitting Parameters and Synthetic Lattice Preferred Orientation (LPO) derived from Edge Driven Convection and Mantle Wind Models in Madagascar [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.909406, Supplement to: Rajaonarison, Tahiry A; Stamps, D Sarah; Fishwick, Stewart; Brune, Sascha; Glerum, Anne; Hu, Jingwen (2020): Numerical Modeling of Mantle Flow Beneath Madagascar to Constrain Upper Mantle Rheology Beneath Continental Regions. Journal of Geophysical Research: Solid Earth, 125(2), e2019JB018560, https://doi.org/10.1029/2019JB018560
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Abstract:
We provide model outputs from "Numerical Modeling of Mantle Flow beneath Madagascar to Constrain Upper Mantle Rheology Beneath Continental Regions" submitted to Journal of Geophysical Research, Solid-Earth. The model outputs are 6 spreadsheets which contain calculated splitting parameters and TI axes or synthetic Lattice Preferred Orientations (LPO) derived from 3 regional mantle flow models in Madagascar: Edge Driven Convection (EDC) model, lithosphere-mantle wind model from Behn et al. (2004), and lithosphere-mantle wind model from Forte et al. (2010):
1. model1_splitting parameters.xlsx: calculated splitting parameters derived from Edge Driven Convection (EDC) at individual stations formatted as: Stations name, longitude [◦], latitude[◦], calculated fast azimuth φcalc[◦], calculated fast azimuth standard deviation [◦], and delay time δt [sec].
2. model2_splitting parameters.xlsx: calculated splitting parameters derived from lithosphere-mantle wind of Behn et al. (2004) at individual stations formatted as: Stations name, longitude [◦], latitude[◦], calculated fast azimuth φcalc[◦], calculated fast azimuth standard deviation [◦], and delay time δt [sec].
3. model3_splitting parameters.xlsx: calculated splitting parameters derived from lithosphere-mantle wind of Forte et al. (2010) at individual stations formatted as: Stations name, longitude [◦], latitude[◦], calculated fast azimuth φcalc[◦], calculated fast azimuth standard deviation [◦], and delay time δt [sec].
4. model1_TI axis.xlsx: calculated EDC-derived TI axes at individual seismic stations and at regular grids of 0.5◦×0.5◦. The file is formatted as longitude [◦], latitude[◦], depth [km], azimuth [◦], and percentage anisotropy [%].
5. "model2_TI axis.xlsx": calculated TI axes derived from lithosphere-mantle wind of Behn et al. (2004) at individual seismic stations and at regular grids of 0.5◦×0.5◦. The file is formatted as longitude [◦], latitude[◦], depth [km], azimuth [◦] , and percentage anisotropy [%].
6. "model3_TI axis.xlsx": calculated TI axes derived from lithosphere-mantle wind of Forte et al. (2010) at individual seismic stations and at regular grids of 0.5◦×0.5◦. The file is formatted as longitude [◦], latitude[◦], depth [km], azimuth [◦], and percentage anisotropy [%].
Coverage:
Latitude: -19.000000 * Longitude: 46.000000
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | File content | Content | Rajaonarison, Tahiry A | |||
2 | File name | File name | Rajaonarison, Tahiry A | |||
3 | File format | File format | Rajaonarison, Tahiry A | |||
4 | File size | File size | kByte | Rajaonarison, Tahiry A | ||
5 | Uniform resource locator/link to file | URL file | Rajaonarison, Tahiry A |
License:
Creative Commons Attribution 4.0 International (CC-BY-4.0)
Size:
30 data points