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- W2027037109 abstract "Abstract The presence of multiple sets of curved and/or non-coaxial slip lineations on a single fault surface suggests changing stress conditions during the movement history of the fault. Curved slip lineations suggest a progressive change in the stress field during a single displacement event, whereas non-coaxial slip lineations suggest periodic reactivation of a fault under different stress conditions. If the direction of slip is assumed to reflect the direction of maximum shear stress acting on a pre-existing fault, changes in only the relative magnitudes of principal stresses acting on the thrust sheet are sufficient to cause changes in slip-lineation orientation. Consequently, curved and/or non-coaxial slip lineations simply may record temporal changes in principal-stress magnitudes resulting from syntectonic erosion, changes in tectonic-stress magnitude, and ramping of thrusts to shallower depths. We illustrate that a decrease in overburden or an increase in the magnitude of tectonic stress results in a progressive up-dip rotation of slip lineations on a fault surface, a rotation which could be misinterpreted as indicating polyphase deformation caused by changes in regional displacement directions. Changes in pore pressure do not influence the trajectory of slip on a fault surface, but rather affect the conditions governing the likelihood for slip to occur." @default.
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- W2027037109 date "1991-09-01" @default.
- W2027037109 modified "2023-09-27" @default.
- W2027037109 title "Factors controlling slip-lineation orientation on thrust-fault planes" @default.
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- W2027037109 doi "https://doi.org/10.1016/0040-1951(91)90297-6" @default.
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