Group A, Poster #137, Fault and Rupture Mechanics (FARM)
Quantifying the Effects of Absolute Friction on Thrust Fault Rupture
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Poster Presentation
2023 SCEC Annual Meeting, Poster #137, SCEC Contribution #12921 VIEW PDF
that their difference remains constant, (b) holding dynamic friction at 0.1 while varying the static friction, and (c) holding static friction at 0.6 while varying the dynamic friction.
For each friction configuration, three models are conducted: (1) a strongly asymmetric case where the upper fault tip terminates at the free surface; (2) a moderately asymmetric case where the upper fault tip is buried 9 km (a blind thrust in a half-space); and (3) an essentially symmetric case where the upper fault tip is buried 120 km (a fault effectively in a whole-space).
Preliminary results for a purely symmetric fault in a whole-space (case 3) demonstrate that different frictional and stress parameterizations produce identical displacements. Thus, only the drop in friction contributes to slip for our model in this case. For the models that approach the free surface, where free-surface-induced normal stress variation is apparent, we find that the evolution of fault rupture and slip does depend on the absolute level of friction. Increasing the frictional coefficients leads to an increase in normal stress feedback and slip, where the effect is dominated by the dynamic friction.
Our findings demonstrate how friction and geometry together affect the temporal evolution of slip and stress on asymmetric faults.
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For each friction configuration, three models are conducted: (1) a strongly asymmetric case where the upper fault tip terminates at the free surface; (2) a moderately asymmetric case where the upper fault tip is buried 9 km (a blind thrust in a half-space); and (3) an essentially symmetric case where the upper fault tip is buried 120 km (a fault effectively in a whole-space).
Preliminary results for a purely symmetric fault in a whole-space (case 3) demonstrate that different frictional and stress parameterizations produce identical displacements. Thus, only the drop in friction contributes to slip for our model in this case. For the models that approach the free surface, where free-surface-induced normal stress variation is apparent, we find that the evolution of fault rupture and slip does depend on the absolute level of friction. Increasing the frictional coefficients leads to an increase in normal stress feedback and slip, where the effect is dominated by the dynamic friction.
Our findings demonstrate how friction and geometry together affect the temporal evolution of slip and stress on asymmetric faults.
SHOW MORE