Basal Solling Sandstone Member RNSOB


Premise Member defined by van Adrichem Boogaert & Kouwe (1994).
Type section Location map See figure (pdf)
  Well L02-01 (pdf)
  Location N 53°57’14.0
E 04°30’47.0
  Depth 3964 to 3970 m
  Length 6 m along hole
Additional section Location map See figure (pdf)
  Well Eleveld-101 (pdf)
  Location N 52°57’27.9
E 06°34’41.9
  Depth 2513 to 2515 m
  Length 2 m along hole
  Well Strijen West-1 (pdf)
  Location N 51°44’41.0
E 04°31’14.3
  Depth 2532 to 2535 m
  Length 3 m along hole
Definition This unit consists of a light-coloured sandstone interval which has a characteristic expression, particularly on the electric logs (high resistivity). In the vicinity of the Cleaver Bank High and the Netherlands Swell, the sandstone generally is absent or too thin to be be distinguished separately. The sandstone is massive or cross-bedded, and dolomite-cemented. Along the basin margin, where sandy sediments prevail, it may be hard to discern the base of the Basal Solling Sandstone Member. If necessary, this unit may be lumped with the mainly sandy Main Buntsandstein Subgroup into the informal Middle Bunter sandstone.
References See References Triassic

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