In lithostratigraphy, coal measures are coal-bearing strata, with the term typically applied to European units of the Upper Carboniferous System.
In the United Kingdom, the term is equivalent to regional components of the Westphalian-age Coal Measures Group. The group records the deposition of fluvio-deltaic sediments which consists mainly of clastic rocks (claystones, shales, siltstones, sandstones, conglomerates) interstratified with the beds of coal. In most places, the coal measures are underlain by coarser clastic sequences known as Millstone Grit, of Namurian age. The top of the coal measures may be marked by an unconformity, the overlying rocks being Permian or later in age. In some parts of Britain, however, the coal measures grade up into mainly coal-barren red beds of late Westphalian and possibly Stephanian age.[1][2] Within the Pennine Basin, these barren measures are now referred to as the Warwickshire Group, from the district where they achieve their thickest development.[3]
The coal measures formed during Westphalian and earliest Stephanian times in the European ('Heerlen') chronostratigraphical scheme (which is approximately equivalent to the Middle Pennsylvanian Series of the IUGS global chronostratigraphical scheme).
- ^ Rayner, D H; Hemingway, J E (1974), The Geology and Mineral Resources Of Yorkshire, Leeds: Yorkshire Geological Society
- ^ Edwards, W; Trotter, F M (1954), The Pennines and Adjacent Areas, British Regional Geology (Third ed.), London: HMSO. Natural Environment Research Council
- ^ Powell, J.; Chisholm, J.; Bridge, D.; Rees, J.; Glover, B.W.; Besly, B.M. (2000). "Stratigraphical framework for Westphalian to Early Permian red-bed successions of the Pennine Basin" (PDF). British Geological Survey Research Report. RR/00/01. Retrieved 13 November 2021.