Sentence examples for deep segment from inspiring English sources

In contrast, the deep segment of the 2011 Tohoku earthquake had been seismically active with large repeating earthquakes of about M 7.5.

The reported sol gel structure was fabricated in a chosen location of our device by selectively retaining sodium silicate solution within a sub-micrometer deep segment via capillary forces, and then providing the precursor material appropriate thermal treatment.

(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).

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.

From the hypocenter relocation image obtained by Hurukawa et al. (2008) and the observed periodicities of earthquakes in the seismic regime, it is highly probable that the next strong shock will be generated by around 2010 in the deep segment (depth: 140 160 km) of the Vrancea focal volume.

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.