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Tectonics
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===Strike-slip tectonics=== [[File:Aerial-SanAndreas-CarrizoPlain.jpg|thumb|[[San Andreas Fault|San Andreas transform fault]] on the [[Carrizo Plain]]]] {{Main article|Strike-slip tectonics}} Strike-slip tectonics is associated with the relative lateral movement of parts of the crust or the lithosphere. This type of tectonics is found along oceanic and continental [[transform fault]]s which connect offset segments of [[mid-ocean ridge]]s. Strike-slip tectonics also occurs at lateral offsets in extensional and [[thrust fault]] systems. In areas involved with [[Continental collision|plate collisions]] strike-slip deformation occurs in the over-riding plate in zones of oblique collision and accommodates deformation in the [[Foreland basin|foreland]] to a collisional belt.<ref name="Burg_2017">{{Cite web |last=Burg |first=J.-P. |date=2017 |title=Strike-slip and Oblique-slip tectonics |url=https://www.files.ethz.ch/structuralgeology/jpb/files/english/5wrench.pdf |access-date=26 September 2022}}</ref>
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