RUSSIAN JOURNAL OF EARTH SCIENCES, VOL. 16, ES3003, doi:10.2205/2016ES000573, 2016 Figure 6. Rose diagrams illustrating the ODF of different mineral fractions as resulted from the analysis of Figure 2 images. Black corresponds to biotite platelets, while dark grey, light grey and white could be attributed to plagioclase and quartz. In all cases the anisotropy parameter has a value of about 2, while both Rayleigh $R$ and Rao's $U$ tests point towards with a 99% probability of a non-uniform, anisotropic distribution of different minerals that compose samples. Copyright 2016 by the Geophysical Center RAS. Generated from LaTeX source by ELXpaper, v.1.5 software package. |