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- W1972280618 abstract "The Lower Permian Yellow Sands are preserved as eight relatively wide draa ridges (linear compound dunes) separated by interdraa corridors at the base of the Marl Slate (Zechstein). Flat-bedded interdraa and draa plinth deposits are a significant constituent of the deposits exposed in the draa ridges. These sediments are composed of relatively coarse-grained wind-ripple strata and form up to 9 m thick tabular sand-bodies. Interdraa deposits are generally the most coarse-grained and are horizontally to sub-horizontally stratified; they are gradationally overlain by low-angle draa plinth deposits with numerous low-angle diastems. The contact between draa plinth and overlying trough cross-bedded draa centre deposits is frequently gradational, but can also be characterized by deep aeolian scours. Each draa ridge contains two interdraa-draa plinth-draa centre units, which record an early phase of lateral migration of the draa field followed by a second phase of vertical accretion." @default.
- W1972280618 created "2016-06-24" @default.
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- W1972280618 date "1989-11-01" @default.
- W1972280618 modified "2023-10-16" @default.
- W1972280618 title "Preservation of interdraa and plinth deposits by the lateral migration of large linear draas (Lower Permian Yellow Sands, northeast England)" @default.
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- W1972280618 doi "https://doi.org/10.1016/0037-0738(89)90011-0" @default.
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