Fig. 6
From: Crystal plasticity as an indicator of the viscous-brittle transition in magmas
Box-plot of deformation intensity across sample sets. The spread in misorientation per micron (simply the lattice distortion (in degrees) divided by the crystal length (in microns)) for a COLB2 and b COLLAH4. This shows the maximum, minimum (the top and bottom ends of the vertical lines), median (the central horizontal line), the 25th and 75th percentiles (the bottom and top of the boxes, respectively) and mean (crosses) of the values for the starting material, each stress and strain (ε) condition and the broken microlites. Using the misorientation per micron allows us to exclude any bias that would result from comparing microlites of different sizes
