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Petrophysical constraints on the seismic properties of the Kaapvaal craton mantle root

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Figure

Fig. 1. Sketch displaying the location of the sampled kimberlitic pipes as well as the samples’ depths and microstructures (after Baptisteet al., 2012) relatively to the S wave tomography model of Fouch et al
Table 1. Olivine Mg#, modal contents, equilibration conditions, calculated seismic properties and densities of the studied Kaapvaal peri-dotites.
Fig. 2. Calculated seismic properties of the Kaapvaal coarse-grained and sheared peridotites showing different olivine CPO patterns
Fig. 3.s) on the olivine CPO strength (characterized by theFigure 3 P,anisotropy (AV Dependence of the maximumBaptiste and Tommasi S1 and S2 wave anisotropies (AVp, AVS1 and AVS2), and of the maximum S wave polarization J index), the olivine content and the BA index.
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