Aalburg Formation

The information on this page is a summary description.
The full formal description is available here: Aalburg Formation

Abbreviation
Parent unit Altena Group
Child units
Lithological description Open marine, grey to dark grey, locally sandy or silty mudstones and marls. Macrofossils (ammonites, molluscs), often pyritised, and siderite nodules can be common. Top: erosive, cut by Mid Cimmerian unconformity and covered by Upper Cretaceous deposits; base: passing inconspicuously into Steen Formation.
Age Lower Jurassic, Hettangian (identified in well KB99) to Pliensbachian (identified in well KB198).
Thickness ca. 450 m preserved thickness in Molenbeersel (becoming thicker and more complete towards the northwest on Dutch territory).
Area of occurrence Roer Valley Graben ; removed by erosion from Campine Basin and eastern Brabant Massif . Aalburg and Sleen Formations follow Pangaea break-up and deposi tion in the North Sea – North German Shale basin during the Rhaetian to Hettangian transgression (Ziegler, 1990).
Type locality Parastratotypes in Belgium: well KB99 Neeroeteren , well KB198 Molenbeersel.
Alternative names
Authors Dusar, M., Langenaeker, V. & Wouters, L.
Date 01/01/2001
Cite as Dusar, M., Langenaeker, V. & Wouters, L., 2001. The Aalburg Formation, 01/01/2001. National Commission for Stratigraphy Belgium. http://ncs.naturalsciences.be/lithostratigraphy/Aalburg-Formation
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