The information on this page is a summary description.
The full formal description is available here: Neuville Member
| Abbreviation | NEU |
| Parent unit | Marche-en-Famenne Formation |
| Child units | none |
| Lithological description | Brown shale with carbonate nodules and beds and lenses of red to grey limestone. Fossils are locally very abundant, notably near the red marble lenses. |
| Age | Terminal Middle Frasnian to Late Frasnian |
| Thickness | 16-24 m in the stratotype section |
| Area of occurrence | Dinant Synclinorium and Durbuy-Philippeville Anticlinorium. |
| Type locality | railway trench sections of the CouvinCharleroi railway line west-south-west of Neuville. |
| Alternative names | none |
| Authors | Mottequin, B., Denayer, J., Delcambre, B., Marion, J.-M. & Poty, E. |
| Date | 23/09/2025 |
| Cite as | Mottequin, B., Denayer, J., Delcambre, B., Marion, J.-M. & Poty, E., 2025. The Neuville Member, 23/09/2025. National Commission for Stratigraphy Belgium. https://ncs.naturalsciences.be/lithostratigraphy/Neuville-Member |
| Additional information |
