Code
DCDN
Status
Formal (Van Adrichem Boogaert & Kouwe 1995).
Lithologische beschrijving
Interval of thick, massive, white, coarse-grained to pebbly, arkosic sandstones with kaolinitic cement, interbedded with some variegated mudstone beds and rare coal seams.
Afzettingsmilieu
Fluvial-fan system. Sandstones: braided fluvial channels and associated overbank sheet floods. And periods of poor flood-plain soil drainage.
Definitie ondergrens
Conformably overlies the Kemperkoul Member. The base is characterised by the abrupt upward transition of dark-coloured coal measures into massive, white sandstones. Seismic data and well-log correlations suggest a slight angular unconformity in the type area.
Definitie bovengrens
Grades into the uppermost part of the Hellevoetsluis Formation and the Strijen Formation towards the central-western part of the Campine Basin.
Dikte indicatie
Up to 300 m in Neerglabbeek-146.
Geografische verbreiding
Regionale correlatie
UK: -; GER: Neeroeteren Formation; BEL: Neeroeteren Formation.
Ouderdom
Moscovian.
Holostratotype
Well:
BBEL0164 (Neeroeteren-113 - KB113 in Belgium)
Depth (thickness) AH:
646 - 692 m (46 m)
Parastratotype
Well:
BBEL0206 (Gruitrode-172, KB172 in Belgium)
Depth (thickness) AH:
770 - 967 m (197 m)
Parastratotype
Well:
BBEL0186 (Neerglabbeek-146, KB146 in Belgium )
Depth (thickness) AH:
730 - 1030 m (300 m)
Oorsprong naam
Named after the Belgian (Campine) village of Neeroeteren, where the type well is situated.
Vorige benaming(en)
None.
Gereviewed door (datum)
Tom van Hoof (2017).
Referenties
Van Adrichem Boogaert, H.A. & Kouwe, W.F.P. 1995. Stratigraphic nomenclature of The Netherlands, revision and update by RGD and NOGEPA, Section C, Silesian. Mededelingen Rijks Geologische Dienst, 50, 1-40.
Cite as
TNO-GDN ([YEAR]). Neeroeteren Formation. In: Stratigraphic Nomenclature of the Netherlands, TNO – Geological Survey of the Netherlands. Accessed on [DATE] from https://www.dinoloket.nl/en/stratigraphic-nomenclature/neeroeteren-formation.