Schistes et Grès Carteret explained

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]

Notes and References

  1. Brasier. M. D.. The Lower Cambrian transgression and glauconite-phosphate facies in western Europe. Journal of the Geological Society. 1 December 1980. 137. 6. 695–703. 10.1144/gsjgs.137.6.0695.
  2. Dore. Francis. La transgression majeure du Paléozoïque inférieur dans le Nord-Est du massif Armoricain. Bulletin de la Société Géologique de France. 1972. S7-XIV. 1-5. 79–93. 10.2113/gssgfbull.S7-XIV.1-5.79.

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