RUSSIAN JOURNAL OF EARTH SCIENCES, VOL. 16, ES2002, doi:10.2205/2016ES000566, 2016


Figure 13. Variations of $V_p$ in mantle xenoliths from the Baikal Rift depending on pressure and orientation of the axes of this xenolith; $a$, $b$, and $c$ are the middle, long, and short of the xenolith, respectively, and $b'$ is a melting zone oriented along the long axis of the xenolith.


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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.


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