2020
DOI: 10.1109/access.2020.2993050
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A Triangulated Irregular Network Constrained Ordinary Kriging Method for Three-Dimensional Modeling of Faulted Geological Surfaces

Abstract: Three-dimensional (3D) modeling of geological surfaces, such as coal seams and strata horizons, from sparsely sampled data collected in the field, is a crucial task in geological modeling. Interpolation is a common approach for this task to construct continuous geological surface models. However, this problem becomes challenging considering the impact of the faults on geological surfaces. Existing methods tend to solve this problem through three steps, including interpolating stratum and fault surface, applyin… Show more

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Cited by 18 publications
(7 citation statements)
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“…Geostatistical analysis methods [13], [14], such as the inverse distance weighting and kriging methods, have been widely used in stratum interpolation for model construction. Jia, QR [15] improved the kriging method, which can be applied to generate a faulted geological surface. Topological information from stratum modeling is another common modeling method that can be used to build a solid model.…”
Section: A Modeling Methods and Toolsmentioning
confidence: 99%
“…Geostatistical analysis methods [13], [14], such as the inverse distance weighting and kriging methods, have been widely used in stratum interpolation for model construction. Jia, QR [15] improved the kriging method, which can be applied to generate a faulted geological surface. Topological information from stratum modeling is another common modeling method that can be used to build a solid model.…”
Section: A Modeling Methods and Toolsmentioning
confidence: 99%
“…. , n} is y(xi), the estimated value of y(x0) at the unsampled position x0 is the weighted sum of value X [23]:…”
Section: Ordinary Krigingmentioning
confidence: 99%
“…Over the past three decades, various modeling theories and techniques have emerged to address the need for 3D models of sedimentary systems. 3D geological modeling methods are generally divided into two categories: explicit and implicit modeling (Jia et al, 2020). Explicit modeling directly defines each object in the model by obtaining the coordinates of key nodes, line segments, and surfaces to establish geological layers (Jessell et al, 2014).…”
Section: Introductionmentioning
confidence: 99%
“…This method demonstrated superior fitting effectiveness over the general inverse distance weighting and ordinary kriging methods, especially when there was significant spatial variability in the borehole data. Jia et al (2020) introduced an ordinary kriging method with Triangulated Irregular Networks (TIN) constraints to construct fault surfaces in geological settings. This method integrates the influence of faults directly into the interpolation process, completing surface modeling in a single stage instead of the traditional two-stage process of interpolating and modifying the surface in the fault area.…”
Section: Introductionmentioning
confidence: 99%