Z2 Fringe Sandstone Member ZEZ2S

 

Premise Member defined by van Adrichem Boogaert & Kouwe (1994).
Type section Location map See figure (pdf)
  Well Q16-02 (pdf)
  Location N 52°07’05.3
E 04°07’15.3
  Depth 3836 to 3851 m
  Length 15 m along hole
Definition The Z2 Fringe Sandstone Member consists of a light-coloured sandstone, fine- to medium-grained and well-cemented with calcite, dolomite and silica cement, and some interbedded claystones that increase in abundance towards the centre of the basin.
Lower Boundary Along the basin fringe, in places where a sandy development prevails, it may be impossible to distinguish the underlying Red-brown Salt Clay Member with certainty. In such cases this unit and the Z2 Sandstone Member may be lumped with the underlying Z1 Sandstone Member into an informal unit: the Zechstein Fringe sandstone (ZEFRS). An example of such a development is found in well Q16-02 (see pdf) , interval 3836 - 3862 m below rt.
References See References Permian

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