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- W329417547 abstract "Alluvial terraces may be used as markers of the deformation across faults. According to faultbend folding theory (Suppe, 1983; Fig. 1), the amount of slip recorded since abandonment of a terrace level may be computed in 3 ways by measuring: 1/ terrace heights on the hanging wall relative to the foot wall (h1, h2), 2/ difference in terrace elevation across the fold scarp (Δh), and 3/ width of the fold scarp (WL), heights and scarp width being independent measurements. Contrary to method 3, methods 1 and 2 require knowledge of the subsurface structure of the fault." @default.
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- W329417547 date "2009-12-01" @default.
- W329417547 modified "2023-09-26" @default.
- W329417547 title "Three Recipes to Decipher Late Pleistocene Slip Rates of the Chelungpu Thrust (Central Taiwan), based on OSL-dated Folded Terraces" @default.
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