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From Source to Surface: The dynamics of heterogeneous mantle plumes

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Figure

Figure 1.1:Fluid model of low viscosity plume rising through a high viscosity environmentillustrating its head-tail structure
Figure 1.2: Maps of large igneous provinces (LIPs). Dotted lines show the known or conjecturedconnections to active volcanic hotspot tracks
Figure 1.3: Injected lab plume that shows location of source versus entrained material
Figure 2.1: The Hawaiian hotspot (green star), plotted above the shear-wave tomography modelS40RTS (Ritsema et al., 2011) at 2800 km depth, illustrating that Hawaii overlies the boundarybetween a large region of low shear-wave velocities – the Pacific LLSVP – and surrounding mantle.Under the assumption that the Pacific LLSVP represents a chemically distinct body, Weis et al.(2011) hypothesise that geochemical differences between the Kea and Loa trends reflect preferentialsampling of these two distinct sources of deep mantle material.
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