Summary
SPani (Tesoniero et al., 2015) is a joint model of radially anisotropic P- and S-velocity variation of the whole mantle based on the inversion of fundamental Rayleigh and Love surface waves up to the sixth overtone and major P- and S-body wave phases. P- and S-sensitive data are coupled in the inversion by Rayleigh wave data and a mineral physics based regularization term on the relationship between S- and P-velocity variation. This page contains supplemental information on this model’s resolution.
Quicklinks
Description
The following images provide information on resolution of the Spani Earth model.
Tables
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Images
Standard checkerboard test
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Checkerboard test designed to evaluate the amount of leakage from the VS model to the VP model
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Resolution test with uncorrelated VP and VS input models
Citations and DOIs
To cite the source of this Earth model:
- Tesoniero, A., Auer, L., Boschi, L., and Cammarano, F. (2015). Hydration of marginal basins and compositional variations within the continental lithospheric mantle inferred from a new global model of shear and compressional velocity. Journal of Geophysical Research: Solid Earth
To reference the use of this Earth model hosted by EMC:
- IRIS DMC (2015), Data Services Products: SPani, 3D joint anisotropic compressional and shear wave velocity model of the whole mantle, https://doi.org/10.17611/DP/EMCSPANI.
To cite IRIS Earth Model Collaboration (EMC) data product or reference use of its repository:
- IRIS DMC (2011), Data Services Products: EMC, A repository of Earth models, https://doi.org/10.17611/DP/EMC.1.
References
- Antolik, M., Gu, Y. J., Ekström, G., and Dziewonski, A. M. (2003). J362D28: a new joint model of compressional and shear velocity in the Earth’s mantle. Geophysical Journal International, 153(2):443-466.
- Ekström, G. (2011). A global model of Love and Rayleigh surface wave dispersion and anisotropy, 25-250 s. Geophysical Journal International, 187(3):1668-1686.
- Ritsema, J., Deuss, A., van Heijst, J., and J.H., W. (2011). S40RTS: a degree-40 shear-velocity model for the mantle from new Rayleigh wave dispersion, tele-
seismic traveltime and normal-mode splitting function measurements. Geophysical Journal International, 184(3):1223-1236. - Ritsema, J. and van Heijst, H. J. (2002). Constraints on the correlation of P- and S-wave velocity heterogeneity in the mantle from P, PP, PPP and PKPab traveltimes. Geophysical Journal International, 149(2):482-489.
- Tesoniero, A., Auer, L., Boschi, L., and Cammarano, F. (2015). Hydration of marginal basins and compositional variations within the continental lithospheric mantle inferred from a new global model of shear and compressional velocity. Journal of Geophysical Research: Solid Earth.
- Visser, K., Trampert, J., and Kennett, B. L. N. (2008). Global anisotropic phase velocity maps for higher mode Love and Rayleigh waves. Geophysical Journal International, 172(3):1016-1032.
Credits
Andrea Tesoniero, Ludwig Auer, Lapo Boschi, Fabio Cammarano