Fig. 2: Sulfur isotopes (δ34S) of troilites in the basalt clasts, breccias and nonmare clasts in CE-6 soil and lunar meteorites analyzed in this study.
From: Sulfur isotopes from the lunar farside reveal global volatile loss following the giant impact
Bulk rock δ34S values of Apollo basalts8,28,29 and CE-5 basalts28,39 are shown for comparison (a). δ34S values and Mg# of associated clinopyroxene are plotted in (b). Data enclosed by the dashed black circle in (b) represent troilites from the same clast or grain. c shows Ni content versus δ³⁴S for the same troilite grain. Error bars represent ±2 standard errors (2SE) of δ³⁴S measurements.
