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Propagation of Pressure Solution Seams

Once initiated from a flaw-like inhomogeneity perpendicular to the greatest compression, the lateral propagation of a pressure solution is dictated by the stress concentration at its tips. In fact, according to the anti-crack model of pressure solution, the intensity of the stress concentration for a closing mode structure is the same as that of an opening mode structure but the signs are opposite (Fletcher and Pollard, 1981; Sternlof et al., 2005). However, Katsman et al. (2006) calculated a lower stress concentration factor for a Localized Volume Reduction Structure. This was later verified by Zhou and Aydin (2010). See some model results provided under 'Mechanisms and Mechanics of Pressure Solution Seams' supporting the tip-stress derived propagation scenario. However, a critical stress intensity factor for the propagation criterion for the lateral propagation of pressure solution seams is not yet known.

Types of Propagation of Pressure Solution Seams:
Anticrack ModelLocalized Volume Reduction Model
Reference:

Fletcher, R.C., Pollard, D.D., 1981. Anticrack model for pressure solution surfaces. Geology 9: 419-424.

Katsman, R., Aharonov, E., Scher, H., 2006. A numerical study on localized volume reduction in elastic media: Some insights on the mechanics of anticracks. Journal of Geophysical Research 111: B03204, doi:10.1029/2004JB003607.

Nenna, F., Aydin, A., 2011. The formation and growth of pressure solution seams in clastic rocks: A field, analytical and numerical study. Journal of Structural Geology 33: 633-643, doi:10.1016/j.jsg.2011.01.014.

Sternlof, K.R., Rudnicki, J.W., Pollard, D.D., 2005. Anticrack inclusion model for compaction bands in sandstone. Journal of Geophysical Research 110: B11403, doi:10.1029/2005JB003764.

Zhou, X., Aydin, A., 2010. Mechanics of pressure solution seam growth and evolution. Journal of Geophysical Research 115: B12207, doi:10.1029/2010JB007614.

Zhou, X., Aydin, A., 2012. Mechanics of the formation of orthogonal sets of solution seams, and solution seams and veins and parallel solution seams and veins. Tectonophysics 532-535, 242-257. http://dx.doi.org/10.1016/j.tecto.2012.02.013.



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