. Author manuscript; available in PMC: 2022 Jan 7.

Published in final edited form as: Geochim Cosmochim Acta. 2020 Nov 1;293:103–126. doi: 10.1016/j.gca.2020.10.025

Table 4.

Host oxygen three isotope ratios of anorthite bearing chondrules.

Chondrule	n	Type	δ¹⁸O	Unc.	δ¹⁷O	Unc.	∆¹⁷O	Unc.	Mg#^a
QUE 97008
c51	7	II-PO	3.89	0.34	2.21	0.25	0.18	0.16	87
c61	7	I-POP	3.96	0.47	2.21	0.27	0.15	0.12	95
c143	8	II-PO	4.83	0.36	2.75	0.21	0.24	0.09	84
c150	8	II-POP	4.54	0.40	2.34	0.35	−0.02	0.32	87
MET 00452
c19	7	II-PO	4.30	0.35	2.14	0.28	−0.10	0.23	83
c111	8	II-POP	4.04	0.33	2.27	0.20	0.17	0.14	90
Semarkona
c34	8	II-POP	4.48	0.33	2.45	0.24	0.12	0.19	82
c47	8	II-PO	4.45	0.35	2.26	0.29	−0.05	0.23	86
NWA 8649
c17	8	I-PP	3.45	0.36	1.36	0.32	−0.44	0.23	93
c87	6	II-PO	3.62	0.40	1.72	0.25	−0.16	0.10	90
NWA 8276
c7	6	II-PO	5.64	0.47	3.29	0.29	0.36	0.17	85
c69	6	I-POP					0.49	0.15	97
c87	8	II-PO	3.59	0.33	1.54	0.22	−0.33	0.13	83
c88	8	II-POP	5.13	0.51	2.81	0.34	0.15	0.20	80

Mg# = Mg / (Mg + Fe) mole%