A left-stepping, generally E-W-striking dextral-normal fault occurs immediately to the south of the dextral fault
(fault B in Figure 6).
This, for example, occurred with the Gafarillos dextral fault
zone to the northeast of the Alhamilla anticlinorium (Fig.
They present findings on the structural geology of dextral fault
zones in the trough, basic analysis and fault activity, and changes after initiation of the San Jacinto and San Felipe fault zones.
Langdon and Hall (1994) interpreted the tectonic structure of the region to be a wrench system involving the major NE-trending faults with minor parallel and cross-cutting dextral fault
arrays and shear zones (i.e., the St.
One WNW-striking dextral fault
plane with a similar fabric was also identified (Fig.
Well exposed latest Devonian--earliest Carboniferous plutons occur along two dextral fault
strands and an en echelon transition zone between them in the southern part of the Cobequid Shear Zone.
The largest measured displacement is 20 m in a dextral fault
striking 080[degrees] in the phyllonite zone on the eastern side of Third Machias Lake.
In the eastern side of KTJ: however, the collision deformation is largely accommodated within the Eastern Anatolian Block through distributed NWSE trending dextral faults
and NE-SW trending sinistral faults representing escape tectonics, and shortening of the continental lithosphere along the Caucasus thrust zone.
Normal, sinistral, and dextral faults
in the same orientations affect both Cambrian and Pennsylvanian rocks.
Most of the faults observed on the surface are strike-slip dextral faults
in addition to more scarce NNW-SSE oriented normal faults.
The main active structures of this fault zone are two ENE-WSW trending reverse blind faults, the Torremendo and Bajo Segura Faults, and three secondary NW-SE dextral faults
, the San Miguel de Salinas, Torrevieja and Guardamar faults.