The information on this page is a summary description.
The full formal description is available here: Kempen Group
Abbreviation
Kp
Parent unit
Child units
Lithological description
The Kempen Group consists of fine grained sandy – clayey sediments which are the result of alternating estuarine and fluvial-eolian conditions at the moment of deposition. It is subdivided into two Formations, namely the Malle Formation and the Weelde Formation.
Age
Thickness
Area of occurrence
Type locality
Alternative names
Authors
Gullentops, F., Bogemans, F., De Moor, G., Paulissen, E. & Pissart, A.
Date
01/01/2001
Cite as
Gullentops, F., Bogemans, F., De Moor, G., Paulissen, E. & Pissart, A., 2001. The Kempen Group, 01/01/2001. National Commission for Stratigraphy Belgium. http://ncs.naturalsciences.be/lithostratigraphy/Kempen-Group