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Time dependent inversion of fault slip.
This paper serves to document the distribution of fault slip of the 1994 Northridge earthquake sequence.
The effect of shear heating-induced thermal pressurization on fault slip.
Bürgmann, R. (2018), The Geophysics, Geology and Mechanics of Slow Fault Slip, Earth Planet.
Kirkpatrick, J. D. et al. Silica gel formation during fault slip: Evidence from the rock record.
Faber, C. et al. Silica gel in a fault slip surface.
Earthquakes have different properties depending on the type of fault slip that causes them (as shown in the figure).
The results of this study have important implications for the modeling of geodetic displacements for fault slip.
Hudnut et al. (1996) and Shen et al. (1996) modeled the fault slip from the static displacement field.
Its slip rate is determined from matching and dating incised Pleistocene alluvial fan deposits and surfaces displaced by fault slip.
This results in quakes in which the two sides of the fault slip past each other without much vertical movement.
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