Sentence examples for fault is lower from inspiring English sources

Based on the current study of seismicity (i.e., the b value of the Gutenberg-Richter (G-R) relationship, where a low value indicates high earthquake activity) upon the Thoen Fault (Lampang Basin) and upon the Phrae Fault (Phrae Basin), the b value for the Thoen Fault is lower than that for the Phrae Fault (Pailoplee et al., 2009).

For the cases in which (300 le sigma_{3} le 440{text{ MPa}}) (including case F), the stress drop (tau^{text{r}} - mu_{text{d}} sigma_{text{n}}^{text{r}}) on the Futagawa fault was lower than 1.5 MPa (lower panel of Fig. 6b).

The aforementioned results show that the rupture velocity of southward faulting is lower than that of northward faulting; furthermore, the rupture length and source duration in the southern fault are also shorter than those in the northern one.

On the other hand, the mega-splay fault branches into several fault planes on the seaward side of the transition zone (Figures 2 and 6), and the reflection amplitudes of the shallow splay faults are lower.

This means that the stacking fault density is lower than ~105 cm-1, and therefore lower than values reported previously, e.g. for A-plane GaN on R-plane Sapphire, 3.83 × 105 cm-1[7].

From the bispectrum amplitudes figure, we can see that the spectral peak amplitude of fault 3 (normal state) is lower than the other four kinds of fault states, because the valve clearance led to changes in the cylinder head trembling of nonlinear features.

An assumption of software fault tolerance techniques is that the probability of having the same fault in multiple variant components is lower, meaning that a fault present in a component should be detected and tolerated based on the behaviour of other variants (Lyu [1996]).

The temperature increase for the case of an intraplate strike-slip fault is much lower than that for an interplate strike-slip fault.

Therefore, the maximum detectable fault resistance in cables is lower than the overhead lines (especially in long cables).

As the rocks above the updip end of the seismogenic zone and above the mid-slope part of the accretionary wedge are not deforming at present, it is inferred that cohesion of fault rocks in the décollement is lower than the values given above.

Recorded time by the second CPSB is compared to the predefined threshold (h1) so that it is detected as symmetrical fault during power swing if it is lower than threshold value.