Sedimentary facies of the Forest Marble (Bathonian), Shipton-on-Cherwell Quarry, Oxfordshire
- 1 March 1973
- journal article
- research article
- Published by Cambridge University Press (CUP) in Geological Magazine
- Vol. 110 (2) , 153-163
- https://doi.org/10.1017/s0016756800047890
Abstract
Summary: The unrivalled exposures of the quarry show the Forest Marble to comprise a complex association of vertically and laterally changing facies. These are interpreted to represent environments ranging from subtidal-intertidal fully marine sand shoals and hard substrates colonized by corals, to mud flats and tidal channels associated with coastal swamps. An earlier interpretation of calcarenites in the Forest Marble is inapplicable at Shipton-on-Cherwell.Keywords
This publication has 3 references indexed in Scilit:
- Bathonian sedimentation in Southern EnglandProceedings of the Geologists' Association, 1967
- Intertidal Zone Channel Deposits in Middle Jurassic Great Oolite Series, Southern EnglandNature, 1963
- The Upper Great Oolite, Bradford Beds and Forest Marble of South Oxfordshire, and the Succession of Gastropod Faunas in the Great OoliteQuarterly Journal of the Geological Society, 1931