Grandcourt Formation

The information on this page is a summary description.
The full formal description is available here: Grandcourt Formation

Abbreviation GRT
Parent unit
Child units
Lithological description Generally bituminous grey clay and marl with a thin silty-calcareous lamination, and laminar limestone nodules (“Schistes Cartons” Member), passing toward the top to sandier laminated marl, rich in septaria. Occurrences of centimetric to decimetric limestone beds.
Age The Grandcourt Formation is dated from Toarcian, from Harpoceras falciferum Zone to Grammoceras thouarcense Zone (Delsate, 1990; Laenen, 1991).
Thickness Thickness of approximately 40 m in the western area. It thickens towards the east to reach about 60 m near the Luxemburg border.
Area of occurrence The formation outcrops in the south of Belgian Lorraine
Type locality Latour borehole.
Alternative names
Authors Boulvain, F., Belanger, I., Delsate, D., Ghysel, P., Godefrout, P., Laloux, M., Monteyne, R. & Roche, M.
Date 01/01/2001
Cite as Boulvain, F., Belanger, I., Delsate, D., Ghysel, P., Godefrout, P., Laloux, M., Monteyne, R. & Roche, M., 2001. The Grandcourt Formation, 01/01/2001. National Commission for Stratigraphy Belgium. http://ncs.naturalsciences.be/lithostratigraphy/Grandcourt-Formation
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