2008
DOI: 10.1144/sp309.2
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Fault seal mapping – incorporating geometric and property uncertainty

Abstract: In this paper, we present workflows, key relationships and results of multiple stochastic fault seal analyses conducted on geocellular geological or (static) reservoir grids. Ranges of uncertainties are computed from new and published datasets for the different input relationships (e.g. throw, VShale to VClay, fault clay prediction, fault rock clay content to permeability); these are used as input into stochastic modelling processes and the impact of each is assessed. The power of stochastic modelling to focus… Show more

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Cited by 16 publications
(6 citation statements)
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References 37 publications
(80 reference statements)
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“…The data also indicate that a range of other factors can influence those relationships; these include burial history (e.g. Sperrevik et al 2002;Freeman et al 2008) and the timing of hydrocarbon migration. With this array of valid but potentially different relationships, it is important to be able to differentiate the most appropriate ones to apply in a given situation, or alternatively to assess what effect selecting different relationships will have on the predicted flow behaviour.…”
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confidence: 88%
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“…The data also indicate that a range of other factors can influence those relationships; these include burial history (e.g. Sperrevik et al 2002;Freeman et al 2008) and the timing of hydrocarbon migration. With this array of valid but potentially different relationships, it is important to be able to differentiate the most appropriate ones to apply in a given situation, or alternatively to assess what effect selecting different relationships will have on the predicted flow behaviour.…”
mentioning
confidence: 88%
“…Yielding 2002) or more commonly as a step toward defining the likely cross-fault permeability, and ultimately the fault TMs for input to flow simulation (e.g. Manzocchi et al 1999Manzocchi et al , 2008Sperrevik et al 2002;Jolley et al 2007;Freeman et al 2008). Fault permeabilities and TMs along the fault surface can then be viewed as values for each cross-fault grid connection (e.g.…”
Section: Visualizing and Interpreting Cross-fault Fluid Flowmentioning
confidence: 99%
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“…The effective crossfault transmissibility (ECFT) is one potential solution (see Figure 1). This property is the total transmissibility of the host rock on one side of the fault, the fault rock and the host rock on the other side of the fault, all normalized to a constant length scale (Freeman et al, 2008). For the same pressure differential, mobility and phase there should be a linear relationship between the ECFT and the fluid flow across the fault.…”
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confidence: 99%