Sentence examples for m in deep from inspiring English sources

Basin of dissipation with drowned jump: 16.5 m in length and 5.5 m in deep (Hydro Projet Ouest 2000).

Great megathrust earthquakes (M w > 8.5) have involved tsunami amplitude greater than 10−1 m in deep seas near the epicenters (Inazu and Saito 2013).

The characteristics of the spillway are: Lateral uncontrolled spillway Flood frequency 1%: 292 m3/s Charge over the threshold: 2.5 m Threshold: length 56 m Trapezoidal channel: 150 m in length and 1.86% in slope Fast channel: 32.5 m in length and 21% in slope Basin of dissipation with drowned jump: 16.5 m in length and 5.5 m in deep (Hydro Projet Ouest 2000).

In the example presented in Fig. 2, the decrease of m in deeper horizons indicates that most of the SOC is associated with smaller aggregate size classes in deeper soil layers.

The estimated slip on the inclined fault surfaces was in the range of 2.0 3.8 m, and the slip was larger on the deeper patches (Fig. 3), with a maximum slip of 3.8 m in the deep northwest patch.

Living at depth exceeding 5,000 m in the deep sea, the strain has to face the two main challenges of low temperature and high hydrostatic pressure.

The present study finds the Umehara fault dipping at 61° toward the southwest, with a maximum slip of 3.8 m in the deep-northwest segment.

From the borehole survey results (Kosaka 2015), there is a slow velocity layer deeper than 10 m, so we added a layer with V s = 110.0 m/s with a thickness of 5 m in the deepest part of the wedge.

The detected ground deformation can be well reproduced using a slip model for the Umehara fault, dipping at 61° toward the southwest, with a maximum slip of 3.8 m in the deeper northwestern segment.

The two-dimensional MT model obtained (after static shift correction) represents resistive bodies (1, 000 3, 000 ohm-m) and conductive bodies (<20 ohm-m) in the deep crust.

The results reveal that the region below the Tapti river shows anomalous high resistivity (1, 000 3, 000 ohm-m) in the deep crustal depths of 20 40 km (R1 in Fig. 5(a)).