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- W2012202034 abstract "Summary The Roman Fell Beds, of hitherto disputed age, are part of the Carboniferous succession of the Roman Fell area. They overlie a basal conglomerate and comprise the Roman Fell Shales and Roman Fell Sandstones, the latter including conglomerates and lithic quartzitic arenites. Thicknesses of these, and of succeeding, beds differ markedly either side of the Swindale Beck Fault along which contemporaneous movement occurred during sedimentation. Roman Fell Sandstones, both north and south of the fault, are petrographically similar; pigmentation by ferric oxides is of secondary origin, unrelated to stratigraphy. Shales with Limestone north of the fault are correlated with the Ravenstonedale Limestones (C 1 —C 2 ), Ashfell Sandstone (S 1 —S 2 ) and Hillbeck Limestone (S 2 ) in a much thicker sequence south of the fault. Petrographical parameters support the stratigraphical interpretations and indicate a gradual change in provenance through the succession, from local outcrops of Ordovician–Silurian rocks during deposition of the basal conglomerate and Roman Fell Beds, to more distant granitic sources during that of the Ashfell Sandstone." @default.
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- W2012202034 date "1967-12-01" @default.
- W2012202034 modified "2023-09-25" @default.
- W2012202034 title "CARBONIFEROUS BASEMENT BEDS IN THE ROMAN FELL DISTRICT, WESTMORLAND" @default.
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- W2012202034 doi "https://doi.org/10.1144/pygs.36.2.203" @default.
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