The information on this page is a summary description.
The full formal description is available here: Ciney Member
| Abbreviation | CIN |
| Parent unit | Condroz Formation |
| Child units | Dorinne Facies, Haversin Facies, Beverire Facies |
| Lithological description | Mixed siliciclastic and calcareous deposits usually rich in brachiopod coquina beds and nodular limestone. |
| Age | Late Famennian |
| Thickness | 200-240 m in the type area. |
| Area of occurrence | Sourthern and western parts of the Dinant Synclinorium. |
| Type locality | The Ciney Member is well exposed along the railway north-west of Leignon. |
| 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 Ciney Member, 23/09/2025. National Commission for Stratigraphy Belgium. https://ncs.naturalsciences.be/lithostratigraphy/Ciney-Member |
| Additional information |
