Abstract
Abstract. Structural geomodeling is a key technology for the visualization and quantification of subsurface systems. Given the limited data and the resulting necessity for geological interpretation to construct these geomodels, uncertainty is pervasive and traditionally unquantified. Probabilistic geomodeling allows for the simulation of uncertainties by automatically constructing geomodel ensembles from perturbed input data sampled from probability distributions. But random sampling of input parameters can lead to construction of geomodels that are unrealistic, either due to modeling artifacts or by not matching known information about the regional geology of the modeled system. We present a method to incorporate geological information in the form of known geomodel topology into stochastic simulations to constrain resulting probabilistic geomodel ensembles using the open-source geomodeling software GemPy. Simulated geomodel realizations are checked against topology information using an approximate Bayesian computation approach to avoid the specification of a likelihood function. We demonstrate how we can infer the posterior distributions of the model parameters using topology information in two experiments: (1) a synthetic geomodel using a rejection sampling scheme (ABC-REJ) to demonstrate the approach and (2) a geomodel of a subset of the Gullfaks field in the North Sea comparing both rejection sampling and a sequential Monte Carlo sampler (ABC-SMC). Possible improvements to processing speed of up to 10.1 times are discussed, focusing on the use of more advanced sampling techniques to avoid the simulation of unfeasible geomodels in the first place. Results demonstrate the feasibility of using topology graphs as a summary statistic to restrict the generation of geomodel ensembles with known geological information and to obtain improved ensembles of probable geomodels which respect the known topology information and exhibit reduced uncertainty using stochastic simulation methods.
Highlights
Structural geomodeling is an elemental part of visualizing and quantifying geological systems (Wellmann and Caumon, 2018)
We show how a single topology graph can be used as a summary statistic in an approximate Bayesian computation (ABC)-rejection scheme to approximate the posterior model ensemble that honors the added information
Simulating the uncertainties encoded in the prior parameterization resulted in 100 unique model topologies within the geomodel ensemble of 2000 models, with 18 topology graphs occurring at least 10 times and the most frequent 14 making up 90 % of geomodel ensemble topologies
Summary
Structural geomodeling is an elemental part of visualizing and quantifying geological systems (Wellmann and Caumon, 2018). As geology is an experimental science, and an interpretive and historical science (Frodeman, 1995), the deduction of the geomodel – often from sparse amounts of data – can inherently lead to numerous potentially valid geological interpretations (Bond et al, 2007), which themselves can lead to numerous topology graphs This aspect is compounded by the complex nature of geological systems and interpretation bias imparted by geoscientists in the explicit creation of geomodels (Bond et al, 2007; Polson and Curtis, 2010; Bond, 2015).
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