Stratigraphic response of salt marshes to slow rates of sea- level changeĬonventional models of salt-marsh development show an idealized spatial relationship between salt-marsh floral and foraminiferal zones, where the landward margin of the marsh gradually migrates inland in response to sea- level rise. Results show the ability of the method to automatically generate stratigraphic correlation scenarios, and also highlight some challenges when sampling stratigraphic uncertainties from multiple wells. To perform cross-validation of the method, we introduce a distance comparing the relative geological time of two models for each geographic position, and we compare the models in terms of volumes. We apply this method on a set of synthetic wells sampling a forward stratigraphic model built with Dionisos. The resulting correlations are then used to create stratigraphic grids in three dimensions. In the presence of multiple wells, this method sequentially updates a stratigraphic column defining the stratigraphic layering for each possible set of realizations.
From an input set of wells, we evaluate the probability for two stratigraphic units to be associated using an analog stratigraphic model. We discuss the sampling and the volumetric impact of stratigraphic correlation uncertainties in basins and reservoirs. Uncertainty management in stratigraphic well correlation and stratigraphic architectures: A training- based methodĮdwards, Jonathan Lallier, Florent Caumon, Guillaume Carpentier, Cédric
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