The Great Oolite Group is a Middle Jurassic stratigraphic unit that outcrops in southern England.
It consists of a complex set of marine deposits primarily mudstone and bioclastic ooidal and fine grained limestone, deposited in nearshore to shelf settings.
[1] It is exposed at the surface as a variably thick belt extending roughly NE-SW from the coast of Dorset up to the Humber.
It is also present at depth in the Weald and Wessex Basins, as well as offshore.
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