Sentence examples for wide fault from inspiring English sources
An 8 cm wide fault was observed at 1046.40 m in the Trumpeters Member sandstone and a 2.5 cm wide fault at 45° to the core axis was encountered at 1121.95 m within the Wonderfontein Member siltstones (Fig. 4).
Multiphase machines have become challenging candidates for safety-critical applications that require wide fault tolerant capabilities and higher system reliability.
In turn, high joint densities correlate with narrow fault cores and low joint densities with wide fault cores.
Repeated cycles of fracture and healing may be one mechanism responsible for wide fault zones with multiple fault cores and damage zones.
This phenomenon is well known, of course, but is particularly dramatic when the rupture extends over a wide fault with variable velocity structure.
These results suggest that repeated cycles of fracture and healing may be the main mechanism creating wide fault zones with multiple fault cores and damage zones.
The geomorphological evolution of the Pliocene–Quaternary Auletta basin, a wide fault-bounded depression of the southern Apennines axial zone, Italy, was reconstructed using both DEM-based morphometric analysis and classical morphotectonic investigations.
Other studies, using both seismic [ Anandakrishnan et al., 1998] and gravity [ Bell et al., 1998; Studinger et al., 2001] techniques have also found patchy to thin (<∼300 m) sediments through most of the West Antarctic Rift System with thicker (>1 km) sediments in narrow (20 35 km wide) fault-bounded basins, which are often associated with the onset of ice streams.
The so-called NY SoccerWarz have already spawned hash tags, GPS-assisted snark, and mutual schadenfreude, to name just a few local delicacies – not to mention providing a ready illustration of some of the wider fault lines in the US Soccer lower league system (it's not really a pyramid) – with the Cosmos making what moves they can in the crowded local market, while flying the flag for the NASL.
The 2011 Tohoku earthquake was a subduction-type earthquake that occurred along the entirety of the Japan Trench, and was associated with a 400-km-long and 200-km-wide fault (e.g., Asano et al., 2011).
On the Tc2 terrace riser at Jaishithok, we observed the fault plane with N10°W trending and 80°E dip in the strongly weathered phyllite belonging to the Lesser Himalayan rocks (Fig. 5) and 2.2-m-wide fault breccia along the plane.
