Assessing Uncertainty in Stratigraphic Correlation: A Stochastic Method Based on Dynamic Time Warping - Université de Lorraine
Communication Dans Un Congrès Année : 2014

Assessing Uncertainty in Stratigraphic Correlation: A Stochastic Method Based on Dynamic Time Warping

Résumé

We propose a method to manage uncertainties about the layering of 3D reservoir models, using stochastic correlations of sedimentary units identified along wells, according to the sequence stratigraphy paradigm. A stratigraphic model represents the architecture of the stratigraphic succession of an area. Sequence stratigraphy is a common paradigm in reservoir studies to interpret and correlate local high resolution observations (outcrops, well logs and core samples) and more exhaustive but lower resolution data such as 3D seismic. The incompleteness of these data, their quantity and their varying quality, added to the fact that the processes that control the geometry and the conformability of the sequences are complex and poorly known, lead to uncertainties. The proposed method aims at building stratigraphic models honoring 1D interpretations along wells together with conceptual sequence stratigraphic rules formulated quantitatively as correlation costs. The algorithm chosen is a modified version of the Dynamic Time Warping algorithm. More than finding the best correlation using a set of rules, it handles different orders of sequences, takes in account the conformability of the horizons, and its output is a set of different possible correlations, allowing for generating alternative stratigraphic layerings. This methodology is demonstrated on the Teapot Reservoir, Wyoming.
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Dates et versions

hal-04068794 , version 1 (14-04-2023)

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Jonathan Edwards, Florent Lallier, Guillaume Caumon, Cédric Carpentier. Assessing Uncertainty in Stratigraphic Correlation: A Stochastic Method Based on Dynamic Time Warping. Second EAGE Integrated Reservoir Modelling Conference, EAGE, Nov 2014, Dubai, United Arab Emirates. ⟨10.3997/2214-4609.20147469⟩. ⟨hal-04068794⟩
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