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• W1752156675 abstract "We report for the first time the occurrence of polygonal faults in sandstone, which is compelling given that layer-bound polygonal fault systems have been observed so far only in fine-grained sediments such as clay and chalk. The polygonal faults are shear deformation bands that developed under shallow burial conditions via strain hardening in dm-wide zones. The edges of the polygons are 1–5 m long. The shear deformation bands are organized as conjugate faults along each edge of the polygon and form characteristic horst-like structures. The individual deformation bands have slip magnitudes ranging from a few mm to 1.5 cm; the cumulative average slip magnitude in a zone is up to 10 cm. The deformation bands heaves, in aggregate form, accommodate a small isotropic horizontal extension (strain <0.005). The individual shear deformation bands show abutting T-junctions, veering, curving, and merging where they mechanically interact. Crosscutting relationships are rare. The interactions of the deformation bands are similar to those of mode I opening fractures. The documented fault networks have important implications for evaluating the geometry of km-scale polygonal fault systems in the subsurface, top seal integrity, as well as constraining paleo-tectonic stress regimes." @default.
• W1752156675 created "2016-06-24" @default.
• W1752156675 creator A5031911908 @default.
• W1752156675 creator A5058885437 @default.
• W1752156675 date "2015-12-01" @default.
• W1752156675 modified "2023-10-18" @default.
• W1752156675 title "Polygonal deformation bands" @default.
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• W1752156675 doi "https://doi.org/10.1016/j.jsg.2015.10.003" @default.
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