Sentence examples for deeper segments from inspiring English sources

For inundation depth, the low-complexity models showed an overestimating tendency, especially in the deeper segments of the channel.

Today, it is one of the central concept in designing more accessible formulations for deeper segments of the eyes.

The central and south segments behaved like shallow lakes with strong variability in TP and phytoplankton biomass, whereas two relatively isolated and deeper segments in the north were characterized with less variability in TP and lower phytoplankton biomass.

Deeper segments of the dermis had much thicker elastic components.

First, we emphasize along-dip segmentation of a subduction zone with shallow and deep segments, whereas only along-strike segmentation has previously been considered for subduction zones.

The frequency of reflux in both superficial and deep segments increased with the clinical severity of disease.

To explain the coseismic displacements, we estimated the fault parameters for the southern part of the Neodani fault, and particularly for the Umehara fault, which we divided into four segments (shallow and deep segments for the northwest and southeast parts).

We hypothesize that the deep segments of the Wenchuan fault only partially ruptured during the coseismic rupture process and that the slip deficit is released by aftershocks or aseismic afterslip.

This marks a very clear contrast with the 2011 Tohoku earthquake, as shown in Fig. 1(a): background seismicity is observed in all the deep segments such as Segments B, C and D, but weak or no seismicity is observed in shallow segments such as Segments C′ and D′. Figure 1(b) shows earthquake distributions before and after the 1964 Alaska earthquake.

In addition to the conventional along-strike segmentation, along-dip segmentation of the fault area or subduction zone is an important feature for the Tohoku subduction zone, as indicated by the difference in background seismicity: virtually no seismicity in shallow segments but active with large events repeating in deep segments.

(1) The first M 7 earthquake (M = 7.1 7.9) occurs in a deep segment (depth: 140 160 km) of seismic regions at the beginning of each century (1 16 years).