Lateral variation within a hiatal-conden
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M.E. Williams
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Article
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2002
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John Wiley and Sons
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English
⚖ 459 KB
## Abstract Shallow‐marine sandstone and berthierinic, ooidal, sandy limestone form the Hackness Rock Member (HRM), a Callovian‐age hiatal‐condensed bed in NE England. The HRM was deposited in response to a rise in relative sea‐level. Apart from the major hiatal surfaces represented by two signific