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 | 2026-01-07T08:59:25Z | |
| dc.date.available | 2026-01-07T08:59:25Z | |
| dc.date.issued | 2006-07-01 | |
| dc.date.updated | 2026-01-07T08:59:25Z | |
| 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.extent | 65 p. | |
| dc.format.mimetype | application/pdf | |
| dc.identifier.idgrec | 534705 | |
| dc.identifier.issn | 0149-1423 | |
| dc.identifier.uri | https://hdl.handle.net/2445/225114 | |
| dc.language.iso | eng | |
| dc.publisher | American Association of Petroleum Geologists | |
| dc.relation.isformatof | Versió postprint del document publicat a: https://doi.org/10.1306/02070605112 | |
| dc.relation.ispartof | AAPG Bulletin, 2006, vol. 90, num.7, p. 1003-1029 | |
| dc.relation.uri | https://doi.org/10.1306/02070605112 | |
| dc.rights | (c) American Association of Petroleum Geologists, 2006 | |
| dc.rights.accessRights | info:eu-repo/semantics/openAccess | |
| dc.subject.classification | Sedimentologia | |
| dc.subject.classification | Turbidites | |
| dc.subject.classification | Geologia del petroli | |
| dc.subject.classification | Geoestadística | |
| dc.subject.classification | Fàcies (Geologia) | |
| dc.subject.other | Sedimentology | |
| dc.subject.other | Turbidites | |
| dc.subject.other | Petroleum geology | |
| dc.subject.other | Geostatistics | |
| dc.subject.other | 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 |
Fitxers
Paquet original
1 - 1 de 1