Sentence examples for shallower segment from inspiring English sources

Tissue in the durotomized area shows a shorter and shallower segment of non-exponential "bleaching" (red) while areas with dura intact show "bleaching" curves with more pronounced non-exponential "bleaching" (blue).

Under the agreement, the Cross-Sound Cable Company is required to place the shallow segment at the required depth -- corrective work that Connecticut had blocked.

Note that no M 7 earthquake occurs in the region above the shallow segment (depth: 60– 80 km) because of its shorter length.

(3) The third M 7 earthquake (M = 7.1 7.5) occurs in a shallow segment (depth: 80 110 km) of seismic regions at the end of each century (77 94 years).

(4) The shallow segment of the subduction zone (Segment C′ in Fig. 1(a)) of the 2011 earthquake had been believed to be safe because of its sparse seismicity and the absence of historical records of large earthquakes.

The background seismicity in the shallow segment in the case of the 2011 Tohoku earthquake had been very low, but large slip occurred there in this megathrust earthquake, suggesting that plate coupling there was strong.

A large tsunami earthquake in 1896 in a shallow segment B′ (Kanamori, 1972) and slow or aseismic slip events in Segment B (Kawasaki et al., 2001), as shown by green patches in Fig. 3(a), indicate weak plate coupling in Segments B and B′.

The first M 7 earthquake occurs in a deep segment at the beginning of each century, the second M 7 earthquake occurs in a midst segment in the middle of each century, and the third M 7 earthquake occurs in a shallow segment at the end of each century.

In other subduction zones, segmentation is primarily along-strike, but the along-dip segmentation and the interrelation between deep and shallow segments appear to have played an essential role in the 2011 Tohoku earthquake. Figure 1(a) leads us to the introduction of along-dip segmentation for the 2011 Tohoku earthquake, in order to describe the seismicity preceding it (Uchida et al., 2009).

The interaction between along-dip segments (deep and shallow segments) led to the great 2011 Tohoku earthquake.

Instead, there occurred the 2011 megathrust event of these segments that also involved trench-ward shallow segments.