Research Article

Deformation-Induced and Reaction-Enhanced Permeability in Metabasic Gneisses, Iona, Scotland: Controls and Scales of Retrograde Fluid Movement

Figure 9

Model showing the progressive changes in fluid infiltration history in fractured metabasic and granitic gneisses. Schematic representation of mineral reaction history shown in lower sketches for two areas (A and B) in metabasic gneiss.