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


Figure 7. Schmidt's stereographic projections (lower hemisphere) for olivine porphyroclasts in sample Tam-1 [Koreshkova, 1996]. Isolines are 1, 2, 3, 5, and 7%; 1 and 3 are the long and short axes of the sample, respectively.


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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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