Post-processing of sequential indicator simulation realizations for modeling geologic bodies

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dc.contributor.authorYamamoto, Jorge Kazuo
dc.contributor.authorBarbosa Landim, Paulo Milton
dc.contributor.authorKikuda, Antonio Tadashi
dc.contributor.authorBaptista Leite, Claudio Benedito [UNIFESP]
dc.contributor.authorLopez, Santiago Diaz
dc.contributor.institutionUniversidade de São Paulo (USP)
dc.contributor.institutionUniv Estadual Paulista
dc.contributor.institutionUniversidade Federal de São Paulo (UNIFESP)
dc.date.accessioned2016-01-24T14:39:58Z
dc.date.available2016-01-24T14:39:58Z
dc.date.issued2015-02-01
dc.description.abstractSequential indicator simulation realizations contain unavoidable artifacts that are geologically unrealistic. This happens because unlikely types can be drawn randomly from the cumulative distribution and be assigned to a cell in the simulated model. This cell may then be used as previously simulated data when a cell in its neighborhood is visited during a random walk. the sequential process sometimes results in geologically unrealistic realizations. However, different realizations can reveal hidden features. Each realization contains both reliable geological information and noise that is displayed as unlikely types. This paper proposes applying the averaging filter that is commonly used in seismic reflection data to improve the signal to noise ratio. After applying this filter, all L realizations will be condensed into a single geological model that contains certain and uncertain cells. This average model is then exhaustively sampled for the certain cells, and this new sample is used to post-process the uncertain cells to reduce the uncertainty. This resampling and post-processing procedure can be repeated until the final model is considered to be good enough. the proposed method is tested with a model of a dike that crosscuts two sedimentary units. the synthetic geologic model was sampled with 24 drill holes. the results show that the final geological model with reduced uncertainty reproduces very well the sedimentary units and the orientation of the dike as well. the dike shape is not fully reproduced and still presents uncertainties because of lack of neighbor data.en
dc.description.affiliationUniv São Paulo, Dept Environm & Sedimentary Geol, São Paulo, Brazil
dc.description.affiliationUniv Estadual Paulista, UNESP, Dept Appl Geol, São Paulo, Brazil
dc.description.affiliationUniversidade Federal de São Paulo, São Paulo, Brazil
dc.description.affiliationUnifespUniversidade Federal de São Paulo, ICAQF, Diadema, Brazil
dc.description.sourceWeb of Science
dc.description.sponsorshipPetrobras S.A. within Caracterizacao e modelagem geologica de reservatorios (CARMOD)
dc.description.sponsorshipConselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)
dc.description.sponsorshipCoordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)
dc.format.extent257-266
dc.identifierhttp://dx.doi.org/10.1007/s10596-014-9465-4
dc.identifier.citationComputational Geosciences. Dordrecht: Springer, v. 19, n. 1, p. 257-266, 2015.
dc.identifier.doi10.1007/s10596-014-9465-4
dc.identifier.issn1420-0597
dc.identifier.urihttp://repositorio.unifesp.br/handle/11600/38677
dc.identifier.wosWOS:000353787600015
dc.language.isoeng
dc.publisherSpringer
dc.relation.ispartofComputational Geosciences
dc.rightsinfo:eu-repo/semantics/restrictedAccess
dc.rights.licensehttp://www.springer.com/open+access/authors+rights?SGWID=0-176704-12-683201-0
dc.subjectSequential indicator simulationen
dc.subjectMultiquadric equationsen
dc.subjectUncertainty zoneen
dc.subjectAveraging filteren
dc.subjectResamplingen
dc.subjectPost-processingen
dc.titlePost-processing of sequential indicator simulation realizations for modeling geologic bodiesen
dc.typeinfo:eu-repo/semantics/article
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