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. Author manuscript; available in PMC: 2021 Sep 15.
Published in final edited form as: Geochim Cosmochim Acta. 2015 Feb 14;155:122–153. doi: 10.1016/j.gca.2015.02.004

Fig. 2a-k.

Fig. 2a-k.

187Os/188Os and 187Re/188Os isotope systematics for subsamples of the 11 Apollo 15 and 16 lunar impact melt rocks. Errors (2σ) are as provided in Table 2. No robust isochrons are observed. The black line in each panel denotes a reference isochron that is appropriate for the reported age of the rock. For samples 65095 (j) and 67095 (k) the plots include data for both bulk silicate fractions and individual metal grains as 60016,290b. The red line is the regression of the data and the inset shows the correlation for 187Os/188Os versus 1/Os for subsamples.