Article ID Journal Published Year Pages File Type
9534347 Earth-Science Reviews 2005 18 Pages PDF
Abstract
Failure to resolve low-displacement tips and damage zones leads to underestimates of L, and exclusion of fault drag leads to underestimates of dmax. Measurement of non-central fault traces leads to underestimates of both dmax and L and an underestimate of dmax/L. In this paper, we examine factors that control the measured displacement-fault length relationships of natural faults. We suggest that there may be systematic differences between the dmax/L ratios where length is measured parallel or normal to the displacement vector, and where the growth histories of individual faults vary due to the nature and number of slip events, linkage, and reactivation. Controlling factors also include material properties and fault types. It is explained how each controlling factor contributes to the dmax/L ratio and should be considered in the statistical analysis of fault data.
Related Topics
Physical Sciences and Engineering Earth and Planetary Sciences Geology
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