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• W2429577165 abstract "Inclined heterolithic stratification (IHS) sets are commonly encountered in the host rock of the Alberta oil sands. Important features in petrophysica l properties have been identified with respect to these sets. Remnant shales constrained by the IHS geometries are of primary interest. Trends in the shale fraction and grain size trends (e.g. fining upward, lateral and distal) are also present. These geologic features may have a significant impact on the response to exploitation through steam assisted gravity drainage (SAGD). The IHS sets are derived from lateral accretion architectural elements within a fluvial depositional setting. The bank retreat fluvial model is a simplified process based model of stream meander migration. This model is parameterized by hydraulic parameters and initialized with realistic channel stream lines from the dampened harmonic model. A realistic channel profile with correctly positioned thalweg may be fit to the migrating streamlines. The migration of this channel results in the generation of realistic lateral accretion geometries. Multiple realizations o f the IHS sets may be calculated with the bank retreat model. The result is unconditional surface based IHS set geometry models. Petrophysical properties may be fit to these models. The resulting models may be applied as training images for multiple-point simulation and to assess the impact of IHS geometries and heterogeneities on reservoir response." @default.
• W2429577165 created "2016-06-24" @default.
• W2429577165 creator A5018381025 @default.
• W2429577165 creator A5061964004 @default.
• W2429577165 date "2015-01-01" @default.
• W2429577165 modified "2023-09-26" @default.
• W2429577165 title "Stochastic Modeling of Inclined Heterolithic Stratification With the Bank Retreat Model" @default.
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