Sentence examples for depth of the slab from inspiring English sources

First the temperature distribution over the depth of the slab is estimated for a given fire scenario.

On the other hand, restrained slabs developed localized cracks, oriented perpendicular to the drying surface and extending through the whole depth of the slab.

The depth of the slab was estimated from a deep seismic plane down to ∼500 km depth (International Seismological Centre, 2001) and a plate interface imaged from seismic data by Takahashi et al. (2009).

The initial or incipient delamination, described as occasional separation within the depth of the slab, can be identified through the presence of dominant frequencies associated with the thickness stretch modes from both the bottom of the deck and the delamination.

Note that, because there exists no direct evidence regarding the actual depth and geometry of the plate interface, the iso-depth contours represent the maximum possible depth of the slab surface, which might be a few to ∼10 km beneath the upper surface of the subducting Indian Plate.

The remaining 32-mm depth of the slab is cast and finished the top surface by proper compaction of concrete (BS 5950: Part 4 [1994]) as shown in Figure 4. Open image in new window Figure 4 Cross-section of test specimen.

Iyer et al. (2012) suggested that the double hydrated zone at the depths of the slab mantle, through slab unbending (Fig. 22; Faccenda et al. 2012) and maximum serpentinization at c. 270 °C, may together cause the variations in the observed separation of the double seismic zone.

We therefore expect that epidote and ternary carbonates will play a fundamental role on reactions on the solidus at variable volatile component abundances, for pressure between 3 and 5 GPa, i.e., for depths of the slab typical for the sub-arc at subduction zones.

A belt of upper-plane seismicity in the crust nearly parallel to 80 90 km depth contours of the slab surface has been detected in the cold Pacific slab beneath eastern Japan, and is probably caused by slab crust dehydration with a large H2O production rate.

As indicated by the arrows in Fig. 7a, e, the upper-plane seismic belt becomes deeper locally in the area beneath this arc arc junction and reaches the vicinity of the 110 -km depth contour of the slab's upper surface.

However, the depth of the Philippine Sea slab is almost similar to that of the Moho boundary beneath the faults of Nobi earthquake (Nakajima et al. 2015).