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

<div>Backscattered electron image of epidote vein (ep(v)) cut by granular epidote cataclasite seam (ep(g)). Large amphibole (hbl) in host gneiss cut by hornblende- (hbl-) actinolite (act) cataclasite, relict clasts (arrowed) of which appear within the granular epidote seam.</div>

Geofluids

fig5

Figure 5

Figure 5: Deformation-Induced and Reaction-Enhanced Permeability in Metabasic Gneisses, Iona, Scotland: Controls and Scales of Retrograde Fluid Movement 

Figure 5 | Deformation-Induced and Reaction-Enhanced Permeability in Metabasic Gneisses, Iona, Scotland: Controls and Scales of Retrograde Fluid Movement 