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The comparisons of different slab materials are also given.
(1) There are remnants of subducted slab materials which are stagnant (sim 150 km above the CMB.
Nevertheless, it is estimated that H2O released by the dehydration of slab materials plays an important role in generating intermediate-depth intraslab earthquakes.
The slab materials inside a prescribed guide are forced to descend kinematically, with a uniform velocity of 10 cm/year at the age about 100 Myr.
The basal thermal boundary layer is thicker beneath the subducted slab materials and a 'passive plume' has developed along the subducted slab remnants.
Whether they stagnate or penetrate the 660 km discontinuity, subducted slab materials would descend to the lower mantle and reach the CMB.
Similar(47)
Brocher and others (1999) reinterpreted previously identified Moho reflections in northern California as reflections on fossil slab material (Figure 5).
The large bandwidth waveguides are designed by introducing line defects in photonic crystal slabs, where the material in the line defect has appropriate dispersion properties relative to the photonic crystal slab material surrounding the line defect.
Such studies assume a simple configuration for the fluid and element transport and use a box model for the subducted slab material, mantle wedge, and volcanic rocks, with prescribed elemental fluxes among the 'boxes.'boxes
Our model also shows a low-velocity anomaly continuous from the CMB to at least 400 km above the CMB (Figs. 2, 3c); this could be an upwelling plume that is deflected around the descending cold slab material (Fig. 4).
We interpret these features respectively as: (1) remnants of slab material where the bridgmanite to Mg-post-perovskite phase transition may have occurred within the slab, (2, 3) large amounts of hot and less dense materials beneath the cold Kula or Pacific slab remnants just above the CMB which ascend and form a passive plume upwelling at the edge of the slab remnants.
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