Barnhoorn, AukeBystrom, JBurlini, LKunze, K2015-12-130040-1951http://hdl.handle.net/1885/81372The evolution of microstructure and crystallographic preferred orientation (CPO) during post-deformational annealing was studied on three calcite rock types differing in purity and grain size: Carrara marble (98% calcite, mean grain size of 115 μm), SolnKeywords: annealing; calcite; crustal deformation; limestone; marble; recrystallization Crystallographic preferred orientation; Grain growth; Large strain; Recrystallisation; Torsion200510.1016/j.tecto.2005.04.0082015-12-11