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• W2057329997 abstract "The deformation of a thin viscous layer that has a moving boundary is investigated for comparison with zones of deformation in the continental lithosphere. Exact analytical solutions, for the case of a Newtonian fluid, and approximate solutions, for the case of fluid with power law rheology, show that: When the imposed velocity vector is normal to the boundary (congressional or extensional regime) the deformation field decays away from the boundary with a characteristic length scale 1/3 to 1/10 the wavelength of the imposed boundary velocity distribution for n between 1 and 10, where n is the stress‐strain exponent in the rheology; in contrast, when the imposed velocity vector is parallel to the boundary (transcurrent regime), the length scale of the deformation field is approximately 4 times smaller. In each case these length scales decrease approximately as n −½ . The difference in length scales arises even in the absence of any buoyancy forces acting on thickened or thinned crust; such forces would modify the ratio of length scales, but not sufficiently to affect this result." @default.
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• W2057329997 date "1985-04-10" @default.
• W2057329997 modified "2023-10-13" @default.
• W2057329997 title "Length scales for continental deformation in convergent, divergent, and strike‐slip Environments: Analytical and approximate solutions for a thin viscous sheet model" @default.
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• W2057329997 doi "https://doi.org/10.1029/jb090ib05p03551" @default.
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