strike-slip fault

The quake occurred on what is called a strike-slip fault, where the

As a significant strike-slip fault system, the formation of the Tanlu fault zone, kinematics (Wang, 2006; Wang and Zhou, 2009; Tang et al., 2009; Tang et al., 2010) and tectonic evolution (Gilder et al., 1999; Zhu et al., 2009).

Even though tsunamis are not common with strike-slip fault earthquakes, they do occasionally happen.

A strike-slip fault might have some amount of vertical motion that could displace seawater.

Israel and Jordan both sit on the Syrian-African rift, a strike-slip fault which is geologists believe produces a major earthquake every century or so.

The most significant fault microdisplacements occurred in first half of 2015, when the NNW-SSE sinistral strike-slip fault (in the Skalisty potok Cave--upper entrance) together with the WNW-ESE dextral strike-slip fault (in the Drienovska jaskyna Cave) were reactivated under the transtensional tectonic regime, where the principal maximum compressional axis operated in a NW-SE direction ([[sigma].sub.1]) during this short-lasting period.

The strike-slip fault and karst collapse structures span confining units of the Floridan aquifer system and could provide high permeability passageways for groundwater movement.

Similarly to the Tancheng-Lujiang Fault Zone, the DunhuaMishan Fault Zone is a strike-slip fault zone.

2003; Serpelloni et al., 2007; Nocquet, 2012) produces a crustal deformation of the southeastern Iberian Peninsula where Late Neogene and Quaternary faulting activity is dominated by a large NE-SW left-lateral, strike-slip fault system known as the Eastern Betic Shear Zone (EBSZ) (De Larouziere et al., 1988; Silva et al., 1993) (Fig.

Strike-slip fault is one of the most dangerous earthquake disaster.