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Some Unusual Ripple Marks in Carboniferous Limestone near Spittal, North Northumberland
Published online by Cambridge University Press: 01 May 2009
Abstract
Ripple marks of unusual dimensions are recorded from the Sandbanks Limestone (Middle Limestone Group) at a foreshore locality 3 miles south of Spittal in North Northumberland. The structures are thought to have been formed in a partially cohesive calcareous mudas wave-oscillation ripples which have undergone penecontemporaneous modification.
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