. . . . . "44399277"^^ . . . . . . . . . . . . . . . . "15444"^^ . . . "Strain partitioning"@en . . . . . . . "Strain partitioning is commonly referred to as a deformation process in which the total strain experienced on a rock, area, or region, is heterogeneously distributed in terms of the strain intensity and strain type (i.e. pure shear, simple shear, ). This process is observed on a range of scales spanning from the grain \u2013 crystal scale to the plate \u2013 lithospheric scale, and occurs in both the brittle and plastic deformation regimes. The manner and intensity by which strain is distributed are controlled by a number of factors listed below."@en . . . . . . . . . . "Strain partitioning is commonly referred to as a deformation process in which the total strain experienced on a rock, area, or region, is heterogeneously distributed in terms of the strain intensity and strain type (i.e. pure shear, simple shear, ). This process is observed on a range of scales spanning from the grain \u2013 crystal scale to the plate \u2013 lithospheric scale, and occurs in both the brittle and plastic deformation regimes. The manner and intensity by which strain is distributed are controlled by a number of factors listed below."@en . . . . . . . . . . "1120069611"^^ . . .