Süntel Formation

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Sub-unitsSand-Tonkomplex & Unterbank Members
Süntel Formation
Stratigraphic range: Kimmeridgian
~155–151 Ma
Süntel Formation at Langenberg quarry
TypeGeological formation
Sub-unitsSand-Tonkomplex & Unterbank Members
UnderliesGigas-Schichten & Holzen Formation
OverliesKorallenoolith Formation
ThicknessVariable, over 60 m (200 ft) at Langenberg Quarry
Lithology
PrimaryLimestone
OtherSandstone, claystone, marl
Location
Coordinates52°18′N 8°48′E / 52.3°N 8.8°E / 52.3; 8.8
Approximate paleocoordinates43°24′N 16°54′E / 43.4°N 16.9°E / 43.4; 16.9
RegionNordrhein-Westfalen, Niedersachsen
CountryGermany
ExtentLower Saxony Basin
Type section
Named forSüntel
LocationLower Saxon Hills
RegionNiedersachsen
Süntel Formation is located in Germany
Süntel Formation
Süntel Formation (Germany)

The Süntel Formation, previously known as the Kimmeridge Formation (German: "Mittlerer Kimmeridge"; Middle Kimmeridge),[1] is a geological formation in Germany. It is Late Jurassic in age, spanning the early to late Kimmeridgian stage. It predominantly consists of limestone deposited in shallow marine carbonate ramp conditions.[2]

Map of the Lower Saxon Hills with Süntel center-right

The formation is part of the Lower Saxony Basin that borders the Süntel massif of the Lower Saxon Hills, part of the larger Harz Mountains. The formation is described as alternations of glauconitic marl, limestone and sandstone.[3]

Paleontological significance

See also

References

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