2
2016.
Morphology of seismically slow lower-mantle structures – Supporting Information
The high degree of inter-model agreement shown in the vote maps and cross sections may be misinterpreted to suggest VS (or VP ) uniformity within the clusters. In fact, velocities vary within the fast and slow families, across different anomalies, and with depth in the mantle. To give the reader a sense of these variations, we plot contours for m=4 on top of the mean velocities across the five S wave tomographic models used here and mask out regions with disagreement across votes ( Figures S4, S5 and S6).