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

Figure 6. Olivine pole figures for sample Tim1-2, Lanzarote Island, Canary Islands [Koreshkova, 1996]. 1 and 3 are the long and short axes of the xenolith, respectively. The horizontal line indicates the foliation plane. The lineation coincides with the long axis of the xenolith. Schmidt's stereographic projection, lower hemisphere. Contours are to 1, 2, 3, 5, and 7%.

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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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