Skip to main content
. 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 39.

Figure 39.

Correlations of Os versus HSE and 187Os/188Os in a combined dataset of > 750 planetary materials discussed in this study. The HSE span up to ten orders of magnitude abundance variations, between iron meteorites and mare basalts, lunar crustal samples and some eucrites that have extremely low abundances of the HSE. Note strong deviations from correlations for some iron meteorites, probably reflecting liquid metal–solid metal partitioning. CC = carbonaceous chondrite; EC = enstatite chondrite; OC = ordinary chondrite; HED = howardite–eucrite-diogenite meteorite.