To account for material slips at microscopic scale, we take deformation mappings as SBV functions varphi , which are orientation-preserving outside a jump set taken to be two-dimensional and rectifiable. For their distributional derivative F=Dvarphi we examine the common multiplicative decomposition F=F^{e}F^{p} into so-called elastic and plastic factors, the latter a measure. Then, we consider a polyconvex energy with respect to F^{e}, augmented by the measure |textrm{curl},F^{p}|. For this type of energy we prove the existence of minimizers in the space of SBV maps. We avoid self-penetration of matter. Our analysis rests on a representation of the slip system in terms of currents (in the sense of geometric measure theory) with both mathbb {Z}^{3} and mathbb {R}^{3} valued multiplicity. The two choices make sense at different spatial scales; they describe separate but not alternative modeling options. The first one is particularly significant for periodic crystalline materials at a lattice level. The latter covers a more general setting and requires to account for an energy extra term involving the slip boundary size. We include a generalized (and weak) tangency condition; the resulting setting embraces gliding and cross-slip mechanisms. The possible highly articulate structure of the jump set allows one to consider also the resulting setting even as an approximation of climbing mechanisms.
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