Muschelkalk Formation

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

Abbreviation
Parent unit Altena Group
Child units
Lithological description Alternation of carbonates, evaporites and fine-grained detrital rocks, deposited in shallow marine to restricted lagoonal conditions. A three-fold yet unnamed subdivision can be made, from bottom to top: 1. variegated mudstones and thin bedded carbonates with anhydrite beds; 2. alternating limestones and dolomites with red clay intercalations and anhydrite; 3. variegated calcareous mudstones and clayey siltstones with anhydrite nodules. Top: passing into Keuper Formation; base: overlying Röt Formation.
Age Middle Triassic, Anisian – Ladinian.
Thickness 85 m.
Area of occurrence Roer Valley Graben; removed by erosion from Campine Basin.
Type locality Parastratotype in Belgium : well KB99 Neeroeteren.
Alternative names
Authors Dusar, M., Langenaeker, V. & Wouters, L.
Date 01/01/2001
Cite as Dusar, M., Langenaeker, V. & Wouters, L., 2001. The Muschelkalk Formation, 01/01/2001. National Commission for Stratigraphy Belgium. http://ncs.naturalsciences.be/lithostratigraphy/Muschelkalk-Formation
We are using cookies to give you the best experience. You can find out more about which cookies we are using or switch them off in privacy settings.
AcceptPrivacy Settings

GDPR