2008
DOI: 10.1016/j.pepi.2008.06.013
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Geological modelling from field data and geological knowledge

Abstract: An original method has been developed to model geology using the location of the geological interfaces and orientation data from structural field. Both types of data are cokriged to interpolate a continuous 3D potential-field scalar function describing the geometry of the geology. Geology contact locations set the position of reference isovalues while orientation data are the gradients of the scalar function. Geometry of geological bodies is achieved by discretising reference isovalues. Faults are modelled usi… Show more

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Cited by 392 publications
(134 citation statements)
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References 18 publications
(9 reference statements)
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“…Conversely, the dispersion function of interpreted measurements (using geophysics) would be expected to be dependent on the sensitivity of the intermediary method. Additionally, dispersion functions may be probabilistic as well as deterministic (Bucher, 2012). Determinism is a strong assumption when no metrological study was conducted beforehand to assess its plausibility.…”
Section: Discussionmentioning
confidence: 99%
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“…Conversely, the dispersion function of interpreted measurements (using geophysics) would be expected to be dependent on the sensitivity of the intermediary method. Additionally, dispersion functions may be probabilistic as well as deterministic (Bucher, 2012). Determinism is a strong assumption when no metrological study was conducted beforehand to assess its plausibility.…”
Section: Discussionmentioning
confidence: 99%
“…Scedasticity is essentially an untouched subject in geological 3-D modeling and it was pointed out to make the geological 3-D modeling community aware of this fact and its potentially nefarious influence on MCUE outputs. However, standard metrological studies can determine scedasticity and include it in a dispersion function to be a parameter of the prior uncertainty distributions (Bewoor and Kulkarni, 2009;Bucher, 2012). The evidence brought at the theoretical and practical levels allows us to strongly advocate for the use of pole vectors over dip vectors.…”
Section: Discussionmentioning
confidence: 99%
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“…This choice is motivated by critical differences between the three approaches, both at the conceptual and practical level (Aug 2004). Geometric modeling engines interpolate features from sparse structural data and topological assumptions (Aug et al 2005;Jessell et al 2014a); they require prior knowledge of topology and are computationally affordable (Lajaunie et al 1997;Calcagno et al 2008). More specifically, explicit geometric engines require full expert 10 knowledge while implicit ones are based on observed field data and topological constraints (Jessell et al 2014a).…”
Section: Mcue Methodsmentioning
confidence: 99%
“…The regional 3D geological models [32], as well as fundamental structures have been simulated by these methods, including folds, faults [33], reservoir structure inverted from dynamic fluid flow response [34], domes [35], and multilayered structures. Some software packages, such as the TProGS package, produce stochastic geological realizations through Sequential Indicator Simulation [36].…”
Section: Related Workmentioning
confidence: 99%