Research Article

Sources and Effects of Fluids in Continental Retrograde Shear Zones: Insights from the Kuckaus Mylonite Zone, Namibia

Figure 9

Mass changes (a) and δ18O values (b) against distance from local high-strain zones. The largest mass change occurs closer to the high-strain zones. Proximity to the local high-strain zones does not seem to affect the δ18O value.