Fig. 5From: Interplay of irreversible reactions and deformation: a case of hydrofracturing in the rodingite–serpentinite systemCompositional cross section across the reaction zone between serpentinite and rodingite (131019-2). In this plot showing variations of Si, Al, Mg, and Fe (apfu) of chlorite, Mg and Si decrease monotonously from serpentinite to rodingite, whereas Al and Fe show reverse trendsBack to article page