Figure 16.
Aspects of the effective transversely isotropy (VTI) component of the oceanic anisotropy model from Data Source 3 is shown with the green dashed line. The red line is our revision of this model in which the moduli A and N are increased so that $(A-C)/2C = (N-L)/2L = 7$ per cent and we tilt the elastic tensor through dip angle $\theta = 45^\circ$. (a) $V_{SV} = L/\rho ^2$. (b) Dip angle $\theta$. (c) S-wave anisotropy, $\gamma = (N-L)/2L$. (d) Ellipticity parameter $\eta _X \equiv 4L/(A+C-2F)$.

Aspects of the effective transversely isotropy (VTI) component of the oceanic anisotropy model from Data Source 3 is shown with the green dashed line. The red line is our revision of this model in which the moduli A and N are increased so that |$(A-C)/2C = (N-L)/2L = 7$| per cent and we tilt the elastic tensor through dip angle |$\theta = 45^\circ$|⁠. (a) |$V_{SV} = L/\rho ^2$|⁠. (b) Dip angle |$\theta$|⁠. (c) S-wave anisotropy, |$\gamma = (N-L)/2L$|⁠. (d) Ellipticity parameter |$\eta _X \equiv 4L/(A+C-2F)$|⁠.

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