Changes

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file:AlHawajAlQahtaniFigure5.jpg|{{figure number|5}}Schematic 3D geometry of salt structures rising from a) line sources and b) point sources. Note the complexity in all directions resulting from salt deformation.‎<ref name=HudecandJackson_2007>Hudec, M. R., and M. P. Jackson, 2007, Terra infirma: Understanding salt tectonics: Earth-Science Reviews, v. 82, no. 1-2, p. 1-28.</ref>]]

file:AlHawajAlQahtaniFigure5.jpg|{{figure number|5}}Schematic 3D geometry of salt structures rising from a) line sources and b) point sources. Note the complexity in all directions resulting from salt deformation.‎<ref name=HudecandJackson_2007>Hudec, M. R., and M. P. Jackson, 2007, Terra infirma: Understanding salt tectonics: Earth-Science Reviews, v. 82, no. 1-2, p. 1-28.</ref>

file:AlHawajAlQahtaniFigure6.jpg|{{figure number|6}}Examples from the deep-water Niger Delta of using channel geometry to constrain strike-slip displacement.‎<ref name=Durandriardetal_2013>Durand-Riard, P., J. H. Shaw, A., Plesch, and G. Lufadeju, 2013, Enabling 3-D geomechanical restoration of strike-and oblique-slip faults using geological constraints, with applications to the deep-water Niger Delta: Journal of Structural Geology, v. 48, p. 33-44.</ref> A) Faulted horizon surface. The small black box is the location of B-E. B-D) Channels lateral geometry on different horizon levels. E) Restoration using the channels geometry to constrain strike-slip displacement. F) Faulted horizon surface. The small black box is the location of G & H. G) Channels lateral geometry on different horizon levels. H) Restored state.]]

file:AlHawajAlQahtaniFigure6.jpg|{{figure number|6}}Examples from the deep-water Niger Delta of using channel geometry to constrain strike-slip displacement.‎<ref name=Durandriardetal_2013>Durand-Riard, P., J. H. Shaw, A., Plesch, and G. Lufadeju, 2013, Enabling 3-D geomechanical restoration of strike-and oblique-slip faults using geological constraints, with applications to the deep-water Niger Delta: Journal of Structural Geology, v. 48, p. 33-44.</ref> A) Faulted horizon surface. The small black box is the location of B-E. B-D) Channels lateral geometry on different horizon levels. E) Restoration using the channels geometry to constrain strike-slip displacement. F) Faulted horizon surface. The small black box is the location of G & H. G) Channels lateral geometry on different horizon levels. H) Restored state.

===Salt tectonics===

===Salt tectonics===