Fig. 6From: Fluid-driven low-grade metamorphism in polydeformed rocks of Avalonia (Arisaig Group, Nova Scotia, Canada)Pole figures showing the orientation of (002) planes of chlorite crystals in the analyzed samples. The colour is related with diffraction intensity and represents the amount of crystals oriented in the same direction. The maximum colour intensity corresponds to the strongest preferential orientation of the crystalsBack to article page