“…The final degree of freedom relates to the hydrostatic strain, which cannot be measured directly but can be determined by constraining the surface normal stress to zero (Wilkinson et al, 2006b). Subsequent methodological refinements have focused on assessing and improving the accuracy and precision of strain measurement and extending the potential applications to more challenging microstructures (Britton, Maurice, et al, 2010;, 2012bBritton et al, 2013aBritton et al, , 2013bMaurice & Fortunier, 2008;Maurice et al, 2012;Plancher et al, 2015;Tong et al, 2015;Villert et al, 2009;Wilkinson et al, 2014). A recent advance that is particularly important for analysis of geological materials, which are commonly deformed to large plastic strains, has been the development of routines for mapping elastic strains in the presence of lattice rotations of several degrees, such as subgrain boundaries , 2012bMaurice et al, 2012).…”