A quantitative analysis of an Upper Westphalian fluviodeltaic succession and a comparison with earlier Westphalian deposits in the Kent Coalfield
William Alfred Read
Abstract
William Alfred Read
Abstract
Summary The Upper Westphalian succession in the National Coal Board's Eastling Wood Borehole, 1976 ‘TR 6303 1472’ has been analysed in terms of upward-fining and upward-coarsening semicycles, transition probabilities and entropies. This analysis confirms that the succession can be divided into a lower coal facies, which like the earlier Westphalian deposits of Kent was laid down dominantly in deltas but which includes numerous channel-fills, and an upper channel facies laid down in a more upstream fluvial environment.
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Summary The Upper Westphalian succession in the National Coal Board's Eastling Wood Borehole, 1976 ‘TR 6303 1472’ has been analysed in terms of upward-fining and upward-coarsening semicycles, transition probabilities and entropies. This analysis confirms that the succession can be divided into a lower coal facies, which like the earlier Westphalian deposits of Kent was laid down dominantly in deltas but which includes numerous channel-fills, and an upper channel facies laid down in a more upstream fluvial environment.
Key concepts: Westphalian sovereignty, Facies, Geology, Ecological succession, Fluvial, Paleontology, Coal measures, Borehole