The information on this page is a summary description.
The full formal description is available here: Champ du Fau Member
| Abbreviation | CHF |
| Parent unit | Bovesse Formation |
| Child units | none |
| Lithological description | Grey shale with brachiopods and some carbonate nodules. |
| Age | Early Frasnian |
| Thickness | Variable, between 10 and 40 m, depending on the development of the underlying member. |
| Area of occurrence | Brabant Parautochthon, from the Dendre River to the Mehaigne River valley. |
| Type locality | The historical outcrops of the Bovesse area have disappeared long ago. Parastratotypes have been selected for each member in the Mehaigne River valley. |
| 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 Champ du Fau Member, 23/09/2025. National Commission for Stratigraphy Belgium. https://ncs.naturalsciences.be/lithostratigraphy/Champ-du-Fau-Member |
| Additional information |
