Fig. 2From: Geochemical constrains on dolomitization pathways of the Upper Jurassic carbonate rocks in the Geneva Basin (Switzerland and France)Photomicrographs of the main facies observed in the Kimmeridgian–Tithonian limestones of the Geneva Basin. a packstone to grainstone facies in the Calcaire de Tabalcon unit; b dolomitized boundstone in the Calcaires de Tabalcon unit; c medium sized, fabric destructive, sucrosic dolomite in the Calcaires de Tabalcon unit; d wackestone with microsolenoid coralsin the Calcaires Récifaux unit; e oncoid grainstone with calcite spar cement in the Calcaires de Landaize unit and f fine to medium sized, fabric destructive, sucrosic dolomite in the Tidalites de Vouglans unit. On the left, the complex, vuggy, porosity is filtered in red and amounts to 12.5% of the total imageBack to article page