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

Figure 3

Map of area D, including the sampled transect (A-B) with sample locations and δ¹⁸O values and schematic cross-section (C-D). Colours are the same as in Figure 2. Dashed lines on the map marks the boundary between protomylonite and mylonite. The ultramylonites are too thin to mark with dashed lines. Rock descriptions and GPS locations can be found in Table S1.