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- DictionaryStrike-slip fault/ˈstrīk ˌslip ˌfôlt/
noun
- 1. a fault in which rock strata are displaced mainly in a horizontal direction, parallel to the line of the fault.
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Geological fault
- strike fault noun : a geological fault whose trend coincides approximately with the strike of associated strata
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Strike and dip. A fault is a planar geologic structure. Like any planar structure, it has an orientation that may be characterized by strike and dip. For small faults, it may be possible to walk up to an outcrop and measure the orientation with a clinometer.
Faults which move horizontally are known as strike-slip faults and are classified as either right-lateral or left-lateral. Faults which show both dip-slip and strike-slip motion are known as oblique-slip faults.
Nov 28, 2023 · Strike-Slip Fault: Strike-slip faults primarily involve horizontal movement along the fault plane. These faults can be further classified as right-lateral or left-lateral, depending on the direction of horizontal movement when facing the fault.
Mar 26, 2021 · A fault is a plane or linear zone of displacement, where rocks on one side of the plane slip past those on the other side. They represent the brittle failure of rock when strain rates are high, a condition usually associated with earthquakes. They form at Earth’s surface and at any depth in the crust where brittle failure is possible.
The meaning of STRIKE FAULT is a geological fault whose trend coincides approximately with the strike of associated strata.
Strike-slip faults are most commonly associated with transform plate boundaries and are prevalent in transform fracture zones along mid-ocean ridges. In pure strike-slip motion, fault blocks on either side of the fault do not move up or down relative to each other, rather move laterally, side to side.
Nov 21, 2023 · A strike-slip fault is formed by shear stress, which occurs whenever two blocks of rock slide past one another. The hanging wall does not lie above or below the footwall at a strike-slip...
