Importance of crustal corrections in the development of a new global model of radial anisotropy
By Mark Panning, V. Lekić, Barbara Romanowicz. 2010
168 citations recorded by the source corpus.
Subfields: Geophysics
View Paper: https://www.semanticscholar.org/paper/c2bfc754edcbe6ccf44e8d15412841971c6270c2
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In Geophysics
- Thorsten W. Becker
- Barbara Romanowicz
- G. Ekström
- V. Lekić
- J. Ritsema
- P. Moulik
- T. Nissen‐Meyer
- Ludwig M. Auer
Citations in the corpus
- Inferring upper-mantle structure by full waveform tomography with the spectral element method (2011, methodology): “…obtain the expressions for group velocity kernels, we start by expressing U in terms of c and (∂c/∂ω)m, and differentiate the expression with respect to m. Reorganizing, we obtain expressions for the group velocity kernels( ∂U ∂m ) ω = U 2 c2 [( 2c U − 1 )( ∂c ∂m ) ω + ω ( ∂ ∂ω ) m ( ∂c ∂m ) ω ] .”
- Savani: A variable resolution whole‐mantle model of anisotropic shear velocity variations based on multiple data sets (2014, methodology): “One can choose amongst a wide variety of basis function to adequately describe a model: lateral and vertical splines [e.g., Panning et al., 2010; Kustowski et al., 2008; Nettles and Dziewoński, 2008; French et al., 2013; Boschi et al., 2004], spherical harmonics [e.g., Ritsema et al., 2011;…”
- Joint inversion for global isotropic and radially anisotropic mantle structure including crustal thickness perturbations (2015, methodology): “S362WMANI +M [Moulik and Ekström, 2014], SAW642ANb [Panning et al., 2010], S40RTS [Ritsema et al., 2011], and SAVANI [Auer et al., 2014] are whole-mantle S velocity models based on surface wave and body wave data, while SEMum2 [French et al., 2013] and SL2013sv [Schaeffer and Lebedev, 2013] are…”
- An anisotropic shear velocity model of the Earth's mantle using normal modes, body waves, surface waves and long-period waveforms (2014, methodology): “The second pre-2008 model, SAW642AN (Panning & Romanowicz 2006), and its successor, SAW642ANb (Panning et al. 2010), were determined using three-component surface- and body wave waveforms using non-linear asymptotic mode-coupling theory.”