All FRP-strengthened slabs failed by de-bonding, however, the extent of de-bonding and the ability of the slab to sustain load post-initiation of de-bonding was dependent on the position of the load.
Numerical models [ Faccenda et al., 2012] and seismic observations [ Ranero et al., 2003; Ranero and Sallarès, 2004] suggest that the normal faulting, due the bending of the slab at the trench, may extent until 20 40 km of depth, allowing a deep hydration of the slab.
Brains were removed from the cranium and cut into 4 5 mm coronal slabs of tissue containing the entire rostrocaudal extent of the hippocampus.
The brains were removed from the cranium and cut into 4 5 mm coronal slabs of tissue containing the entire rostrocaudal extent of the SVZ.
The extent of the slab slab contact area, which is enclosed by two thick, broken green lines in Fig. 7a, corresponds approximately to the extent of the Kanto Plain. Figure 7a shows that the down-dip end of the contact area is parallel to the upper-plane seismic belt, adjacent to its shallow side, and oblique to the 70 90 -km depth contours of the upper surface of the slab.
Next, we compute for each such volume slab the projection extent on the detector, combined for the full range of projection angles; this is the region of the detector that is affected by an FP of the slab (in any projection direction), or, equivalently, the region of the detector that affects a BP to the slab.
Diffusion element of the slab model.
The depth at which the slab dehydrates depends on many factors that influence the thermal structure of the subduction zone, such as slab age, slab dip, subduction velocity, but also on the lithology of the slab and initial water content.
Because the slab system provides two independent surfaces, an incoming molecule was placed on both sides of the slab.
Bond network arguments suggest that the octahedra at the surface of the slabs should be more distorted than those at the center of the slab.
