Fig. 7From: The North Penninic Bündnerschiefer and Flysch of the Prättigau (Swiss Alps) revisitedMicrophotos of thin sections. Note that as few metamorphic or sheared examples as possible are shown. Qz quartz, Qp polycrystalline quartz, P plagioclase, Musc muscovite, Bio biotite, Dolo dolomite lithoklast, Ech Echinoderm fragment, Fe-Cc iron-bearing calcite. A Quartz-bearing limestone bed of the Klus Formation; thin section stained for carbonate under normal light; echinoderm fragments (brownish-red) in iron-bearing sparitic calcite cement (blue); uncoloured grains are corroded quartz. B Spongy limestone from the Klus Formation under normal light. C Relatively coarse-grained sandstone from the Valzeina Formation (+ Nicols) consisting of quartz, plagioclase and muscovite; brownish grains are dolomite clasts. D Coarse sandstone in the lower part of the Sassauna Formation; besides quartz and corroded plagioclase, the calcite-cemented sandstone is rich in muscovite; + Nicols. E Thin section stained for feldspars from the Pfävigrat Formation; + Nicols; pinkish plagioclase is visible next to dominant quartz. F Carbonate-stained sandstone from the Pfävigrat Formation with similar characteristics as shown in A; here brownish-grey fine-sparitic to micritic dolomite lithoclasts can be seen. G Coarse arkose sandstone coloured for feldspars from the Fadura Formation; polarised light; plagioclase appears greyish pink, quartz is uncoloured; the matrix is siliceous and an incipient formation of fibrous beards is visible in the pressure shadows of the quartz grains. H Sublitharenite from the Gyrenspitz Formation; quartz dominates among the terrigenous grains, plagioclase and polycrystalline lithoclasts make up about 10% each; sparitic ferruginous cement; + Nicols. I Globotruncana linneiana in a sandstone of the Gyrenspitz Formation (pers. comm. M. Caron, Université de Fribourg, 2021). J Arkose from the Eggberg Formation, stained for carbonate under normal light; ferrous calcite cement (blue) and fibrous beards in the pressure shadows of the quartz grains. K Subarkose from the upper part of Oberälpli Formation; + Nicols. L Quartz-rich feldspathic litharenite of the Ruchberg Formation; stained for feldspar and under crossed Nicols. Quartz grains (grey to white) and plagioclase (pink) embedded in sparitic calcite cementBack to article page