Holocene slip rate of the Wasatch fault zone, Utah, from geodetic data: Earthquake cycle effects

Physics

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Tectonophysics: Dynamics, Seismotectonics, Tectonophysics: Continental Tectonics-Extensional (0905), Seismology: Seismic Hazard Assessment And Prediction, Geodesy And Gravity: Crustal Movements-Interplate (8155), Geodesy And Gravity: Rheology Of The Lithosphere And Mantle (8160)

Scientific paper

GPS data define a broad zone of present day deformation in the eastern Basin and Range province, western US. Using finite element models with elastic upper crust over viscoelastic lower crust/upper mantle and incorporating earthquake cycle effects, we show that these data are consistent with a model whereby most contemporary fault slip is focused on the Wasatch fault zone. Modeled rates of horizontal extension are 3.0-4.5 mm/yr, in agreement with Holocene geologic data. The models are non-unique, in part because much of the Wasatch fault is in the late stages of the earthquake cycle, when surface velocity gradients across the fault are low.

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