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- W405950774 abstract "An almost complete section through the Mercia Mudstone Group is exposed in the cliffsbetween Sidmouth and Axmouth on the south Devon coast. This is the only section inNorth West Europe that exposes such a complete sequence of the mid to late Triassic'Keuper Marl' facies. The c. 450.m-thick succession dips gently eastwards in a series oflong, continuous sections that are separated from one another by minor faults which, withone exception, do not cut out any of the succession. At Seaton about 50 m of strata occurwithin a complexly faulted zone in which fault-bounded fragments of the successioncannot be readily correlated with the main outcrop. The availability of a continuous corefrom a nearby borehole has enabled the sequence in the faulted section to be piecedtogether for the first time, and to provide a complete stratigraphy for the group. Thepreviously un-named lower part of the Mercia Mudstone Group (the beds below the BlueAnchor Formation) exposed in the Devon coastal sections can be divided into threeformations and nine members based on gross lithology. The lowest and highest of theseformations consists of relatively monotonous red mudstones for which the namesSidmouth Mudstone and Branscombe Mudstone are proposed. The middle formation, forwhich the name Dunscombe Mudstone is proposed, consists of a 35 m-thick sequence oflaminated green, purple and grey mudstones which expands in some inland successionsproved in boreholes to over 100 m by the addition of thick beds of salt. The lithologiesexposed in the coastal sections can be correlated with the geophysical-log signatures of theMercia Mudstone Group successions proved in inland boreholes throughout the WessexBasin." @default.
- W405950774 created "2016-06-24" @default.
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- W405950774 date "2001-01-01" @default.
- W405950774 modified "2023-09-26" @default.
- W405950774 title "The lithostratigraphy of the Mercia Mudstone Group (mid-late Triassic) of the south Devon coast" @default.
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