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- W133838843 abstract "The subdivision of the Mercia Mudstone Group in south-west England into fourformations (the Sidmouth, Dunscombe and Branscombe mudstones and the BlueAnchor Formation) and nine members, each with a distinctive suite of geophysicallogsignatures, has made it possible to identify lateral lithological variations within thegroup. Prominent among these are halite-rich beds that are almost wholly confined tothe Dunscombe Mudstone Formation. Their distribution is related to major faults inthe underlying Variscan basement that gave rise to differential subsidence during thedeposition of the Mercia Mudstone Group. Up to 30 m of halite is present within theDunscombe Mudstone Formation in the Central Somerset Basin between theQuantock Hills and Mendip Hills structural highs, and up to 130 m of halite is presentin the Wessex Basin on the south side of the Cranborne–Fordingbridge structuralhigh. Thick beds of halite are absent from the Dunscombe Mudstone Formation overthese structural highs and over a subsidiary structure that runs from the QuantockHills to the east Devon coast between Sidmouth and the Axe Valley. Thin beds ofcollapse breccia in the Dunscombe Mudstone Formation in coastal exposures in eastDevon may be residues derived from thin beds of halite." @default.
- W133838843 created "2016-06-24" @default.
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- W133838843 date "2004-01-01" @default.
- W133838843 modified "2023-09-26" @default.
- W133838843 title "The distribution of halite (rock-salt) in the Mercia Mudstone Group (mid to late Triassic) in south-west England" @default.
- W133838843 hasPublicationYear "2004" @default.
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