Code
SKWFF
Status
Formal (NAM & RGD 1980). Amended (Van Adrichem Boogaert & Kouwe 1993).
Lithologische beschrijving
Bluish grey, limestone-rich claystone interval which is characterised by the dominant occurrence of serpulid fragments. The frequently intercalated microcoquina beds and laminae contain abundant pelecypod and ostracod remains. Anhydritic beds and nodules are abundant.
Afzettingsmilieu
Lacustrine basin-margin to marginal-marine sub-basin (lagoonal) setting. With low input of clastic material.
Definitie ondergrens
Usually conformably overlies the Weiteveen Upper Marl Member, but locally unconformably overlies the Altena Group or older sediments.
Definitie bovengrens
Marked by characteristic wire-line log marker, corresponding to conspicuous claystone break in the clayey-marly interval with limestones.
Dikte indicatie
Up to 120 m.
Geografische verbreiding
Regionale correlatie
UK: ?; GER: Serpulit (Münder Formation); BEL: -.
Ouderdom
Berriasian.
Holostratotype
Depth (thickness) AH:
1230 - 1330 m (100 m)
Hypostratotype
Well:
Depth (thickness) AH:
1046 - 1087 m (41 m)
Hypostratotype
Depth (thickness) AH:
1697 - 1708 m (11 m)
Hypostratotype
Well:
Depth (thickness) AH:
1174 - 1218 m (44 m)
Hypostratotype
Well:
Depth (thickness) AH:
295 to 374 m (79 m)
Oorsprong naam
Named after the dominantly occurring serpulite fragments.
Vorige benaming(en)
None.
Gereviewed door (datum)
Sander Houben (2017).
Referenties
NAM & RGD 1980. Stratigraphic nomenclature of The Netherlands. Verhandelingen van het Koninklijk Nederlands Geologisch Mijnbouwkundig Genootschap 32, 77 p.
Van Adrichem Boogaert, H.A. & Kouwe, W.F.P. 1993. Stratigraphic nomenclature of The Netherlands; revision and update by RGD and NOGEPA, Section G, Upper Jurassic and Lower Cretaceous. Mededelingen Rijks Geologische Dienst, 50, 1-80..
Cite as
TNO-GDN ([YEAR]). Serpulite Member. In: Stratigraphic Nomenclature of the Netherlands, TNO – Geological Survey of the Netherlands. Accessed on [DATE] from http://acc.dinoloket.nl/en/stratigraphic-nomenclature/serpulite-member.