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. Author manuscript; available in PMC: 2019 Feb 1.
Published in final edited form as: Int J Mass Spectrom. 2017 Jan 16;414:80–86. doi: 10.1016/j.ijms.2017.01.002

Fig. 1.

Fig. 1.

Measured oxygen isotopic compositions for ReO3− (this study), RuO3− [20], and MoO3− [21]. The oxygen isotopic composition of atmosphere reported by Nier (1950) and a terrestrial fractionation line (dashed-dotted line), which were used by previous studies [14,1] are shown for reference. Linear regressions are shown as dashed (ReO3−), solid (RuO3−), and dotted (MoO3−) lines.