RUSSIAN JOURNAL OF EARTH SCIENCES, VOL. 15, ES1001, doi:10.2205/2015ES000546, 2015
Figure 6. $^{143}$Nd/$^{144}$Nd–$^{87}$Sr/$^{86}$Sr diagram for xenoliths from Tumbusun-Dulga volcano in comparison with analogous data on xenoliths from elsewhere (our data). The black dashed line contours the compositional field of xenoliths from Western and Central Europe [Downes, 2001], and the green dashed line outlines the field of xenoliths from East Asia [Xu et al., 2004]. BSE is the uniform chondritic reservoir.
Citation: Grachev A. F. (2015), Compositional heterogeneity of the continental mantle: Evidence from ultramafic xenoliths in cenozoic basalts from Northern Eurasia, Russ. J. Earth Sci., 15, ES1001, doi:10.2205/2015ES000546.
Copyright 2015 by the Geophysical Center RAS.
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