Schouwen Member CLZLS

 

Premise Unit, defined by Van Adrichem Boogaert and Kouwe (1994).
Derivatio nominis Named after the western part of the island of Schouwen-Duiveland in the province of Zeeland.
Type section Location map See figure (pdf)
  Well S02-02 (pdf)
  Location N 51°51'21.7
E 03°36'32.3
  Depth 2123 to 2604 m
  Length 481 m along hole
Additional section Location map See figure (pdf)
  Well Heugem (pdf)
  Location N 50°49'39.0
E 05°42'50.9
  Depth 114 to 502.7 m
  Length 388.7 m along hole
Definition A thick sequence of light to dark-grey, dark- to yellowish-brown and brownish-black, and light yellowish-brown to dusty yellow-brown limestones. The dense limestones are micritic, biosparitic to biomicritic, locally oolitic and abundantly fossiliferous. In places coarsely crystalline calcite veins occur. Intergranular bituminous, organic material is often present. Locally, the limestones are dolomitized, especially near fault zones, or silicified in the leached zone in areas where later erosion truncated the Zeeland Formation.
Age Middle to late Visean (V2 to V3a; late Arundian to Holkerian), locally even early Visean (V1) in the lower part of the member. The member yielded the diagnostic foraminifers Palaeotextularia, Eotextularia diversa, Eoparastaphella, Dainella, Bessiella, Pseudolituotubella, Archeodiscus (Glomodiscus) and Loeblichia, and the calcareous algae Girvanella densa and Koninckopora.
References See References Upper Carboniferous

Van Adrichem Boogaert, H.A. & Kouwe, W.F.P., 1993-1997. [Stratigraphic unit]. In: Stratigraphic Nomenclature of the Netherlands.
Retrieved [Datum] from [url].