Abstract
Paired comparison models can be used to study the order of stratigraphic events along a relative time scale when differences in order are observed to occur in stratigraphic sections or wells. They give parameters of (1) a binomial distribution for the probability that a given event occurred earlier than another event, or (2) a trinomial distribution for the probability of earlier, later, or simultaneous occurrences of events. In the Bradley-Terry and Davidson models differences in positions of events along a logarithmic scale are assumed to satisfy a logistic frequency distribution. In the recently developed RASC model, a normal frequency distribution along a linear scale is used. The properties of these three models are reviewed and computer algorithms used to obtain practical solutions are discussed. The three models have each been applied to three published data sets (10 highest and lowest occurrences of Eocene nannofossils in 9 wells in California; 16 lowest occurrences of Cambrian trilobites and other fossils in 7 stratigraphic sections in Texas; and 41 highest occurrences of Cenozic foraminifera and other microfossils in 16 wells, Canadian Atlantic Margin). Results of the three models are not significantly different. However, only the RASC model can be applied to large data sets because its computer algorithm avoids the use of timeconsuming iterative processes required when other models are used.
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Contribution to International Geological Correlation Programme Project 148, (Quantitative Stratigraphic Correlation Techniques). Manuscript received 23 March 1981; revised 6 October 1981.
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Hudson, C.B., Agterberg, F.P. Paired comparison models in biostratigraphy. Mathematical Geology 14, 141–159 (1982). https://doi.org/10.1007/BF01083949
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DOI: https://doi.org/10.1007/BF01083949