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- W2017516853 abstract "Shell-detrital calcirudite units occur at a level near the middle of the Forest Marble Formation and are interpreted as shell shoals, shell sheets, tidal channels and tidal deltas. They are considered to separate a facies belt representing an open marine muddy shelf from one representing a sandy, very shallow, possibly somewhat restricted, marine environment. These facies belts become less distinct in the area between Wincanton and Bradford-on-Avon." @default.
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- W2017516853 date "1983-01-01" @default.
- W2017516853 modified "2023-10-18" @default.
- W2017516853 title "The shell-detrital calcirudites of the Forest Marble Formation (Bathonian) of southwest England" @default.
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- W2017516853 doi "https://doi.org/10.1016/s0016-7878(83)80044-3" @default.
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