Abstract:Estimates of fault slip rates are an integral part of assessing seismic hazard because they affect estimates of earthquake renewal and moment release rates. For some faults, however, slip rate estimates vary among geodetic studies or between geodetic and geologic investigations. These differences may reflect time-transient deformation, but they may also reflect differences in spatial scale of observations and in particular a lack of knowledge of how fault geometries change with depth. This study seeks to chara… Show more
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