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Elements; August 2008; v. 4; no. 4; p. 247-252; DOI: 10.2113/GSELEMENTS.4.4.247
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Figure 7


FIGURE 6 Chondrite-normalized PGE abundances measured in basalt-hosted mantle-lherzolite xenoliths collected from five continents. Note that very few analyses match the Becker et al. (2006) primitive mantle estimate. Most xenoliths are significantly depleted in PGE, especially Os. DATA SOURCES: REHKÄMPER ET AL. (1997); HANDLER ANDBENNETT (1999); LORAND AND ALARD (2001); PEARSON ET AL. (2004); BECKER ET AL. (2006)





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