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  • Edge Driven Convection; seismic anisotropy; File content; File format; File name; File size; lattice preferred orientation (LPO); Madagascar; Uniform resource locator/link to file  (1)
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  • Edge Driven Convection; seismic anisotropy; File content; File format; File name; File size; lattice preferred orientation (LPO); Madagascar; Uniform resource locator/link to file  (1)
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    PANGAEA
    In:  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
    Publication Date: 2023-01-13
    Description: 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 [%].
    Keywords: Edge Driven Convection; seismic anisotropy; File content; File format; File name; File size; lattice preferred orientation (LPO); Madagascar; Uniform resource locator/link to file
    Type: Dataset
    Format: text/tab-separated-values, 30 data points
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