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. Author manuscript; available in PMC: 2019 Mar 6.
Published in final edited form as: Rev Mineral Geochem. 2016 Jan 1;81(1):161–238. doi: 10.2138/rmg.2016.81.04

Figure 31.

Figure 31.

(a) CI-chondrite normalized HSE abundances and (b) 187Re/188Os versus 187Os/188Os for lunar crustal rocks, including ferroan anorthosites (FAN) and magnesian suite (MGS) rocks. The MGS includes troctolites (76535), norites (15455, 77215, 78235) and dunites (72415). Data from Day et al. (2010). Shown in (b) is the 4.568 Ga IIIAB iron isochron from Smoliar et al. (1996).