Sentence examples for depth of the upper from inspiring English sources

The depth of the upper Ob (at low water) varies between 6.5 and 20 feet (2 and 6 metres).

The contour lines show the depth of the upper plate interface of the subducted Pacific plate every 20 km.

The thick lines indicate the depth of the upper surface of the subducting Pacific Plate (Kita et al. 2010).

Contour lines overlapping the circles indicate the depth of the upper surface of the Pacific plate (Nakajima and Hasegawa, 2009).

Therefore, the depth of the upper boundary of slab in the offshore areas was estimated using the OBS models.

Since ECr16 is near ECr6, their crustal models are similar to the depth of the upper crustal layer.

A low-velocity layer that corresponds to the slab crust extends down to the depth of the upper-plane seismic belt (A in the figure), and no further.

A recent analysis of P-to-S converted waves under central Tohoku by Shiina et al. (2013) reported that the seismic low-velocity layer persists down to the depth of the upper-plane seismic belt in the subducted oceanic crust.

As also shown in Fig. 8b, the low-velocity layer under Tohoku extends to a depth of approximately 80 km, the depth of the upper-plane seismic belt, and no further.

Estimated P-wave velocity at the depth of the upper-plane seismic belt in the low-velocity crust is c. 10% lower than theoretically predicted values for metamorphosed mid-ocean ridge basalt (MORB).

The seismic low-velocity layer that persists to the depth of the upper-plane seismic belt in the slab crust, as described in the "The double seismic zone and dehydration of metamorphosed crust and 149 serpentinized mantle" section, is one example of such internal structure.