RUSSIAN JOURNAL OF EARTH SCIENCES, VOL. 16, ES2002, doi:10.2205/2016ES000566, 2016
Figure 11. Variations of $V_p$ in mantle xenolith CH-1 from the Bohemian Massif depending on pressure and orientation of the axes of this xenolith; $a$, $b$, and $c$ are the middle, long, and short axes of the xenolith, respectively.
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