The Schistes et Grès Carteret are a series of phosphatic and glauconitic Tommotian siliciclastics exposed in Normandy, France.[1]
They overlie Precambrian conglomerates and are overlain by the Calcaires de Laize.[2]
References edit
- ^ Brasier, M. D. (1 December 1980). "The Lower Cambrian transgression and glauconite-phosphate facies in western Europe". Journal of the Geological Society. 137 (6): 695–703. doi:10.1144/gsjgs.137.6.0695.
- ^ Dore, Francis (1972). "La transgression majeure du Paléozoïque inférieur dans le Nord-Est du massif Armoricain". Bulletin de la Société Géologique de France. S7-XIV (1–5): 79–93. doi:10.2113/gssgfbull.S7-XIV.1-5.79.