Jauche Member

The information on this page is a summary description.
The full formal description is available here: Jauche Member

Abbreviation JAU
Parent unit Chalk group
Child units
Lithological description From bottom to top the Cretaceous strata at Orp-Jauche comprise:
– sands and sandy marls at the base of the white chalks;
– calcarenitic or sandy facies of the white chalk;
– very fine-grained white chalk with black flints;
– coarse-grained chalk with bed with rolled pebbles and nodules at the base;
– calcarenites with Thecidea papillata, flints and a pebble bed at the base;
– unconformably overlain by Palaeocene sands and marls with flint pebbles at the base.
Age The Late Maastrichtian brachiopod Thecidea papillata occurs in great numbers in the Jauche Member.
Thickness 0.20 m to 2 m.
Area of occurrence
Type locality Stratotype: at old quarry at Orp-le-Grand (Orp-Jauche, east Brabant).
Alternative names
Authors Robaszynski, F., Dhondt, A.V. & Jagt, J.W.M.
Date 01/01/2001
Cite as Robaszynski, F., Dhondt, A.V. & Jagt, J.W.M., 2001. The Jauche Member, 01/01/2001. National Commission for Stratigraphy Belgium. https://ncs.naturalsciences.be/lithostratigraphy/Jauche-Member
Additional information Remarks: Previously known as “Tuffeau d’Orp-le-Grand “ in Thielens (1871-1872), Rutot & Van den Broeck (1887-1888), Leriche (1929), Marlière (1957). The denomination “Orp-le-Grand” was used previously by Thielens (1871-1872) for two levels in the section – one of Maastrichtian age and one of Palaeocene age. Vincent (1873) used “Sables heersiens d’Orp- le-Grand” for this Palaeocene formation, generally today called “Sables d’Orp”. Thus, it was necessary to introduce a new name for the Cretaceous lithostratigraphic unit, and since today Orp and Jauche belong to the same administrative unit, it was decided to name it Jauche Member.

Lithostratigraphy Cretaceous

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