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. Author manuscript; available in PMC: 2019 May 1.
Published in final edited form as: Geochim Cosmochim Acta. 2018 Mar 5;228:220–242. doi: 10.1016/j.gca.2018.02.040

Fig. 5.

Fig. 5.

Δ17O values of individual host chondrules in Murchison. Relict olivine grains are shown together. Data are from Tables 1 and 2. The homogeneous chondrule data are sorted following the host Δ17O values. For heterogeneous chondrules (B3, A8, A7, A4, and C10), individual analyses within each chondrule are shown.