The San Andreas and North Anatolian faults are textbook examples of right lateral strike slip faults.
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Both are strike slip faults nearly 1, 000 miles long, storing tremendous energy generated at the confluence of tectonic plates.
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As this takes place, the fault changes from a normal fault with extensional stress to a strike slip fault with lateral stress.
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The numerous strike slip faults in the area could be involved too, whereas subduction of the Tarim Basin beneath the Kunlun is unlikely.
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The dominating feature of the fracture zone is the 150 km long Blanco Ridge, which is a high-angle right-lateral strike slip fault with some component of dip-slip faulting.
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On a larger scale, a zone between offset strike slip faults may have minor " en echelon " fault strands that accommodate the shearing motion induced in the region.
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The syntaxis on either side of the Himalaya are dominated by a strike slip fault zone, instead of a compressional thrust faulting, as in the rest of the orogen.
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A viable method proposed to make room from ascending magma is a zone of lateral extension which can be found at mid ocean ridges, strike slip faults and dialational jogs.
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The formation is bounded on its edges by a series of high-angle strike slip faults, which have contained the Klondike Mountain Formation in a series of graben structures, such as the Republic Graben.
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The "'Septentrional-Orient fault zone "'( SOFZ ) is a system of coaxial left lateral-moving strike slip faults which runs along the northern side of the island of Hispaniola where Haiti and the Dominican Republic are located.
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