A fluvial depositional unit is characterized by a central axis, denoted as a streamline. A set of streamlines can be used to describe a stratigraphic interval. This event-based (denoted as event-based to avoid confusion with streamline-based flow simulation) approach may be applied to construct stochastic fluvial models for a variety of reservoir types, fluvial styles and systems tracts. Prior models are calculated based on all available soft information and then updated efficiently to honor hard well data.
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Pyrcz, M.J., Deutsch, C.V. (2005). Conditioning Event-based Fluvial Models. In: Leuangthong, O., Deutsch, C.V. (eds) Geostatistics Banff 2004. Quantitative Geology and Geostatistics, vol 14. Springer, Dordrecht. https://doi.org/10.1007/978-1-4020-3610-1_14
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DOI: https://doi.org/10.1007/978-1-4020-3610-1_14
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