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- W2063348567 abstract "ABSTRACT The Sutton Stone and Southerndown Beds of the Glamorgan Lias nearshore sediments accumulated around islands of Carboniferous Limestone and are composed predominantly of poorly-sorted lithoclasts of derived chert and limestone in a white to grey calcilutite matrix. Differences between the nearshore Sutton and Southerndown Beds are most pronounced in the matrix character, as determined by field and analyses studies of thin sections, while the color-defined boundary between them may be difficult to delineate. Petrographical study of the offshore limestone-shale sequence indicates that apparent macroscopic homogeneity is not confirmed microscopically. Offshore limestones are calcilutites (micrites) and contain a predominance of molluscan bioclastic debris similar to the faunal debris in s ales and mudstones. Micro-sedimentary variations which can be traced throughout the area emphasize the importance of sediment distribution by currents, but not always widespread environmental stability. Abundant burrowing organisms have disrupted and obscured evidence as to the origin and conditions of deposition of the Blue Lias. The complicated diagenetic history of the sediments is reviewed and summarized." @default.
- W2063348567 created "2016-06-24" @default.
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- W2063348567 date "1965-01-01" @default.
- W2063348567 modified "2023-10-14" @default.
- W2063348567 title "Sedimentology of the Lias (Lower Jurassic) of South Wales" @default.
- W2063348567 doi "https://doi.org/10.1306/74d71325-2b21-11d7-8648000102c1865d" @default.
- W2063348567 hasPublicationYear "1965" @default.
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- W2063348567 hasVolume "Vol. 35" @default.
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