Sentence examples for mechanisms at depth from inspiring English sources

Figure 1 illustrates the four SV mechanisms at depth.

The contributions of the different SV mechanisms at depth and their dependence on the dynamo control parameters are explored.

Of the four radial field SV mechanisms at depth (Fig. 1), radial stretching is the only dynamo mechanism (Oslon et al. 1999, Aubert et al. 2008b).

Stress inversion was applied to focal mechanisms at depths ranging from 50 to 80 km, leading to an acceptable misfit (∼47°).

Also, it can be seen that the faulting type changes from normal to reverse fault type in deeper parts (14 20 km) for the first event, and the variance reduction (VR) does not change so much with these different fault mechanisms at different depths, but the CLVD of the chosen solution with respect to depth is much smaller than other (Figs. 8, 16).

Such tensional stresses are also supported by earthquake mechanisms at shallower depths than 60 km (Fukuyama et al. 1998; Okada et al. 2004), which are mostly normal faulting with trench parallel strikes, around the outer rise region (Fig. 4a).

One can obtain smaller VR by using more stations with a good azimuthal coverage (Yılmazer 2009), which was one of the problems for us to obtain more seismograms during the process of this study and it may be the result of the variation of mechanisms at some depths.

The events with strike-slip mechanism occurred at depths up to 18 km, consistent with the lack of surface rupture in the north-easternmost section.

The Hi-net first-motion solution of this earthquake using a 1D velocity model gave a normal-faulting mechanism at a depth of 18 km, but this is an incorrect solution because of the misestimation of the depth and takeoff angles due to the low-angle dipping slab (Takemura et al. 2016).

According to the MT inversion using observed long-period displacements, the 2016 SE offshore Mie earthquake was characterized by a low-angle thrust faulting mechanism at a depth of 11 km, while the F-net MT solution of this earthquake showed a reverse faulting mechanism with a dip angle of 38° and a depth of 14 km.

Four key technologies were developed to support this system: drill bit development for varied substrates, sample acquisition mechanisms to acquire cores at depth, material transport technologies to move waste material up the hole, and sample reduction technologies, studying the means to efficiently reduce samples into uniform particle sizes.