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

Figure 4. Olivine pole figures for six sections perpendicular to the long axis of xenolith CH-1 from the Bohemian Massif [Grachev et al., 1987]. The arrow in the right-hand part indicates the direction along which the thin sections were marked (Wulf's stereographic projection, upper hemisphere). All diagrams are based on data of 100 measurements.

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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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