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. 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. 5.

Fig. 5.

Oxygen 3-isotope diagram of individual spot analyses of olivine, Low-Ca pyroxene (Lpx), high-Ca pyroxene (Hpx), and relict grains in chondrules in Paris. Error bars, corresponding to the spot-to-spot reproducibility (2SD), are smaller than the symbol sizes. The CCAM (carbonaceous chondrite anhydrous mineral; Clayton et al., 1977), Y&R (Young and Russell, 1998), and PCM (primitive chondrule minerals; Ushikubo et al., 2012) lines are shown for reference. The terrestrial fractionation line (TFL) is also shown.