Best-practice stochastic facies modelling from a channel fill turbidite sandstone analog (the 'Quarry outcrop', Eocene Ainsa Basin, NE Spain)

dc.contributor.author
Falivene Aldea, Oriol
dc.contributor.author
Arbués, Pau
dc.contributor.author
Gardiner, Andy
dc.contributor.author
Pickup, Gillian
dc.contributor.author
Muñoz, J. A.
dc.contributor.author
Cabrera, Lluís
dc.date.accessioned
2026-01-08T21:35:11Z
dc.date.available
2026-01-08T21:35:11Z
dc.date.issued
2026-01-07T08:59:25Z
dc.date.issued
2026-01-07T08:59:25Z
dc.date.issued
2006-07-01
dc.date.issued
2026-01-07T08:59:25Z
dc.identifier
0149-1423
dc.identifier
https://hdl.handle.net/2445/225114
dc.identifier
534705
dc.identifier.uri
http://hdl.handle.net/2445/225114
dc.description.abstract
Using data from an outcrop characterization of a sandstone-rich turbidite channel fill (the so-called ‘‘Quarry outcrop’’ in the Ainsa basin), several stochastic facies models were constructed at bedscale resolution (cells 2.5 m [8 ft] wide and 0.05 m [2 in.] thick).</p><p>Several industry-standard reservoir-modeling algorithms were employed: truncated Gaussian simulation, sequential indicator simulation, multiple-point geostatistics, and object-based methods with varying degrees of complexity. </p><p>The degree of similarity (i.e., realism) between realizations and the outcrop characterization was quantified through the use of several responses: (1) static connectivity, (2) effective permeability, and (3) recovery efficiency from waterflood simulations.</p><p>Differences in the responses measured from the outcrop and facies models were observed: these are mostly algorithm related, instead of caused by soft data or different stochastic realizations. Differences increase greatly when the permeability of the heterolithic</p><p>packages and mudstone beds (Ht-M) decreases and reflect the methods’ ability to model the inclined and undulating Ht-M packages and beds that occur in the outcrop. These packages and beds can drape scours and sandstone beds with depositional topography</p><p>and pinch-outs, producing sandstone thinning and dead ends.</p><p>Object-based methods capable of introducing highly undulating Ht-M beds provided the most realistic models. Variogram-based and simple object-based methods failed to capture and reproduce the whole length of undulating beds. </p><p>Multiple-point geostatistics provided realizations with responses intermediate between variogram-based and simple object-based methods and the more successful advanced object-based methods. The conditioning-to-harddata capabilities of multiple-point geostatistics are higher than those of the object-based methods, which give them an added advantage.
dc.format
65 p.
dc.format
application/pdf
dc.language
eng
dc.publisher
American Association of Petroleum Geologists
dc.relation
Versió postprint del document publicat a: https://doi.org/10.1306/02070605112
dc.relation
AAPG Bulletin, 2006, vol. 90, num.7, p. 1003-1029
dc.relation
https://doi.org/10.1306/02070605112
dc.rights
(c) American Association of Petroleum Geologists, 2006
dc.rights
info:eu-repo/semantics/openAccess
dc.subject
Sedimentologia
dc.subject
Turbidites
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Geologia del petroli
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Geoestadística
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Fàcies (Geologia)
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Sedimentology
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Turbidites
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Petroleum geology
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Geostatistics
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Facies (Geology)
dc.title
Best-practice stochastic facies modelling from a channel fill turbidite sandstone analog (the 'Quarry outcrop', Eocene Ainsa Basin, NE Spain)
dc.type
info:eu-repo/semantics/article
dc.type
info:eu-repo/semantics/acceptedVersion


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