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(a) CI-chondrite normalized HSE abundances and (b) 187Re/188Os versus 187Os/188Os for angrite meteorites. Data from Riches et al. (2012; unfilled circles) and Dale et al. (2012; filled circles). Shown in (b) is the 4.568 Ga IIIAB iron isochron from Smoliar et al. (1996).
