Strike-slip tectonics or wrench tectonics is a type of tectonics that's dominated by lateral (horizontal) movements inside the Earth's crust (and lithosphere). Where a zone of strike-slip tectonics kinds the boundary between two tectonic plates, this is called a remodel or conservative plate boundary. Areas of strike-slip tectonics are characterised by specific deformation kinds together with: stepovers, Riedel
Wood Ranger Power Shears official site, flower structures and strike-slip duplexes. Where the displacement along a zone of strike-slip deviates from parallelism with the zone itself, the style turns into either transpressional or transtensional relying on the sense of deviation. Strike-slip tectonics is characteristic of several geological environments, together with oceanic and continental transform faults, zones of oblique collision and the deforming foreland of zones of continental collision. When strike-slip fault zones develop, they usually type as a number of separate fault segments which can be offset from each other. The areas between the ends of adjacent segments are often known as stepovers.
