Skip to main content
Progress in Earth and Planetary Science
Fig. 7 | Progress in Earth and Planetary Science

Fig. 7

From: Interplay of irreversible reactions and deformation: a case of hydrofracturing in the rodingite–serpentinite system

Fig. 7

Activity diagram showing the saturation lines of diopside and tremolite (solid lines) and that of antigorite (broken line), showing the equilibrium conditions of the minerals under constant activity of Si4+. The arrow indicates a change from the equilibrium point A of diopside and antigorite to that B of tremolite and antigorite within a hydrofractured vein

Back to article page