GEO-MIX-SELF calculations of the elastic properties of a textured graphite sample at different hydrostatic pressures

Matthies, S.

doi:10.1107/S002188981104338X

Figure 5
[gamma]

sections of the orientation distribution function for the graphite sample derived from the experimental pole figures shown in Fig. 2

. Owing to the hexagonal crystal symmetry of single-crystalline graphite, the [gamma]

sections are 60° cyclic, i.e. up to 60° they contain all nonredundant information on the ODF. f_min = 0.402, f_max = 1.995, F₂ = 1.056. Same orientation of the sample coordinate system K_A as in Fig. 2