Verifying the high-order consistency of training images with data for multiple-point geostatistics
Author
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Pérez, Cristian
Author
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Mariethoz, Gregoire
es_CL
Author
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Ortiz Cabrera, Julián
es_CL
Admission date
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2015-01-08T15:20:30Z
Available date
dc.date.available
2015-01-08T15:20:30Z
Publication date
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2014
Cita de ítem
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Computers & Geosciences 70 (2014): 190–205
en_US
Identifier
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dx.doi.org/10.1016/j.cageo.2014.06.001
Identifier
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https://repositorio.uchile.cl/handle/2250/127010
General note
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Artículo de publicación ISI
en_US
Abstract
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Parameter inference is a key aspect of spatial modeling. A major appeal of variograms is that they allow inferring the spatial structure solely based on conditioning data. This is very convenient when the modeler does not have a ready-made geological interpretation. To date, such an easy and automated interpretation is not available in the context of most multiple-point geostatistics applications. Because training images are generally conceptual models, their preparation is often based on subjective criteria of the modeling expert. As a consequence, selection of an appropriate training image is one of the main issues one must face when using multiple-point simulation. This paper addresses the development of a geostatistical tool that addresses two separate problems. It allows (1) ranking training images according to their relative compatibility to the data, and (2) obtaining an absolute measure quantifying the consistency between training image and data in terms of spatial structure. For both, two alternative implementations are developed. The first one computes the frequency of each pattern in each training image. This method is statistically sound but computationally demanding. The second implementation obtains similar results at a lesser computational cost using a direct sampling approach. The applicability of the methodologies is successfully evaluated in two synthetic 2D examples and one real 3D mining example at the Escondida Norte deposit.
en_US
Patrocinador
dc.description.sponsorship
The work presented in this paper was financially supported by the National Fund for Science and Technology of Chile (FONDECYT) as part of the Project number 1090056 and by the National Centre for Groundwater Research and Training (Australia). The support of the ALGES laboratory at the Advanced Mining Technology Centre (Chile) is also acknowledged.