Skip to main content
. Author manuscript; available in PMC: 2021 Nov 12.
Published in final edited form as: Geochim Cosmochim Acta. 2021 Feb 18;299:199–218. doi: 10.1016/j.gca.2021.02.012

Fig. 7.

Fig. 7.

Δ17O values of individual host chondrules in Paris vs. Mg#s (open diamonds). Data from the Murchison CM2 chondrite (black and white squares; Chaumard et al., 2018) are shown for comparison. Chondrule Mg# uncertainties correspond to the range of measured values, while uncertainties in Δ17O are the propagated 2SE.