BreviaDisplacement efficiency of faults and fractures
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Incremental strains measured by incremental crystal growths
Cited by (6)
Geological control of young orogenic mountain morphology: From geomorphological analysis to reinterpretation of geology of the Outer Western Carpathians
2021, GeomorphologyCitation Excerpt :Narrow mountain ridges here have a fan-shaped (broom-like) pattern, with characteristic widening from the vicinity of Žlina towards SW (Mikulov-Bratislava line) (Fig. 3A – site 10). This structure usually compensates for displacements in marginal parts of the strike-slip zone (Fig. 3D – 4) (see Higgs and Williams, 1987; Walley, 1988). Although the flower structure has been described from this region (Beidinger and Decker, 2016), it has not been linked with the horsetail structure reflected in the morphology.
Assessing uncertainties in balanced cross sections
2011, Journal of Structural GeologyCitation Excerpt :Although these are accommodated via minimum shortening estimates in line-length sections, there is a reasonable maximum projection of the hanging wall cutoff as well. If the section of interest lies close to the tip line of an emergent thrust, one could use an up-plunge projection and some model of the displacement gradient profile along a fault (Higgs and Williams, 1987; Marrett and Allmendinger, 1990; Walsh and Watterson, 1987, 1989) to determine where the now eroded hanging wall cutoff should lie. More commonly, we suspect, people will use their intuition as to the probable location of the cutoff and simply select a large uncertainty.
Slip distributions on faults: effects of stress gradients, inelastic deformation, heterogeneous host-rock stiffness, and fault interaction
1994, Journal of Structural GeologyKinematic analysis of fault-slip data
1990, Journal of Structural GeologyDisplacement efficiency of faults and fractures: Discussion
1987, Journal of Structural GeologyDetermination of fault displacement vector parameters based on strike separation
2011, Przeglad Geologiczny