Fig. 5: Evolution of velocities in the rollover subduction models. | Communications Earth & Environment

Fig. 5: Evolution of velocities in the rollover subduction models.

From: Mantle upwelling induced by slab rollover subduction could explain widespread intraplate volcanism in Tibet

Fig. 5

Diagrams illustrating the temporal evolution of velocities for the two rollover subduction models. a Trench velocity (VT in green) and subducting plate velocity (VSP in blue). b Subduction velocity (VS = VSP + VT in black). c Maximum magnitude of mantle upwelling laterally away from the subducting plate (Vup_edge in red) and maximum magnitude of mantle upwelling in the broader mantle wedge domain (Vup_MW in orange). Model rollover_tomo is represented by a continuous line while model rollover_stereo is represented with a dashed line. The black triangles indicate the approximate time at which the slab touches the bottom of the tank. Note that the position of Vup_MW with respect to the trench does not change much, as the distance between them (of the order 500–700 km) remains relatively constant throughout the experiment (cf. Figures 4a, b).

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