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.
Citation: Grachev A. F. (2016), Anisotropy of elastic properties and thermal conductivity of the upper mantle – a case study of xenoliths shape: Evidence from xenoliths in basalts in North Eurasia, Russ. J. Earth Sci., 16, ES2002, doi:10.2205/2016ES000566.
Copyright 2016 by the Geophysical Center RAS.
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