Research Article

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

Figure 7

Scanning electron microscope backscatter electron images of (a) layers of interconnected phyllosilicate networks in a mylonite and (b) a representative ultramylonite depicting a fine-grained mixture, with a random distribution of all constituent phases of the rock. Quartz and albite are dark gray, K-feldspar is light gray, and phyllosilicates are light gray and lamellar shaped. .
(a)
(b)