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Mechanisms and Mechanics of Compaction Band Zones

There are two mechanisms for the formation of the compaction band zones.

First, sequential formation of two or more bands adjacent to each other. Second, the interaction among bands nearby. Please see 'Compaction Band Zones' and 'Echelon Volumetric Bands.'

Figure 1 includes a number of conceptual models depicting how compaction bands are added sequentially to form zones. The total thickness of the zone depends on the architecture of the zone. Sub-parallel bands of equal length (a1 and c1) may be defined by a nearly constant thickness, while sub-parallel bands of different lengths (a2, c2, and c3) may have variable lengths. Field measurements by Torabi et al. (2015) indicate that along most of the zone length (L), except eye structures, the thickness (T) remains almost constant. This arrangement also results in splays of various geometry distributed along the whole zone.

Schematic diagrams illustrating geometry and formation mechanisms of compaction band clustering and widening: (a1 and a2) two sub-parallel bands; (b1 and b2) two bands forming eye structures; (c1 and c2) sub-parallel multiple bands with thickness distributions; and (c3 and c4) imbricated echelon multiple bands with splay bands. Simplified from Torabi et al. (2015).Figure 1. Schematic diagrams illustrating geometry and formation mechanisms of compaction band clustering and widening: (a1 and a2) two sub-parallel bands; (b1 and b2) two bands forming eye structures; (c1 and c2) sub-parallel multiple bands with thickness distributions; and (c3 and c4) imbricated echelon multiple bands with splay bands. Simplified from Torabi et al. (2015).
Reference:

Torabi, A., Aydin, A., Cilona, A., Jarsto, B.E., Deng, S., 2015. The dynamics and interaction of compaction bands in Valley of Fire State Park, Nevada (USA): Implications for their growth, evolution, and geostatistical property. Tectonophysics 657: 113-128. http://dx.doi.org/10.1016/j.tecto.2015.06.029.



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