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- W34174008 abstract "Field evidence from ancient and modern foreland-type thrust belts indicates that several styles of fault slip are involved in the emplacement of external thrust sheets; for example, typical earthquake faulting in the range of 1 m s−1 and fault creep in the range of 10−5-10−6m s−1. Elastic stiffness and velocity-dependent fault damping are two of the fundamental factors that determine whether slip is stable or unstable. The elastic stiffnesses of sedimentary packages depend not only on elastic constants and thicknesses of the strata, but also on the elastic strain gradient with depth. Methods are developed to enable elastic stiffness and velocity-dependent fault damping parameters to be estimated with field data from thrust belts. Quantitative application of these methods is illustrated with the Hogsback thrust sheet in the Kemmerer region of the Wyoming Salient. The data indicate that some of the imbrication of the Hogsback ramp anticline probably had occurred seismically. Data analysis also indicates that the 12 km or more net slip of the Hogsback sheet accumulated principally by recurring slip events with specific rates at least 103 times greater than average geologic slip rates of 10−9-10−10 m s−1." @default.
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- W34174008 date "1992-01-01" @default.
- W34174008 modified "2023-09-27" @default.
- W34174008 title "Chapter 17 Role of Elastic Stiffness and Fault Damping during Thrust-sheet Emplacement in a Foreland Belt" @default.
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- W34174008 doi "https://doi.org/10.1016/s0074-6142(08)62832-6" @default.
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