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, applying a fault modeling method to modify the geological surface, and optimizing the modified surface to pass sample points fallen into the fault displacement zone. This paper presents a more concise method to generate a faulted geological surface, in which 1) a constrained Delaunay triangulated irregular network (CD-TIN) is constructed to facilitate the neighborhood search process of the ordinary kriging (OK) interpolation, 2) the CD-TIN is also directly constrained by horizon cut-off lines formed from theoretical fault displacement profiles, and 3) subsequently, neighbors of the location to be estimated are selected effectively in the CD-TIN considering the fault topology. The proposed method significantly improves the time efficiency of the OK interpolation by utilizing the CD-TIN and incorporates fault effects directly into the interpolation process by inserting fault horizontal cut-off lines into CD-TIN. Moreover, by integrating the fault effects directly into the interpolation process, the surface modeling process is accomplished in a single stage instead of two separate stages of interpolation first and then modifying the surface in the fault area. By this strategy, the proposed method significantly improves the time efficiency of the OK interpolation algorithm and achieves more accurate modeling of the faulted geological surface. Experiments were designed to compare the performance of our method with several commonly used approaches, and the results indicate that the proposed TIN-constrained OK method achieves better accuracy and efficiency in modeling faulted geological surfaces than other methods. This method could also be used in geospatial interpolation studies, such as meteorological data interpolation.

Highlights

  • In subsurface studies, three-dimensional (3D) structural modeling helps geologists understand the physical world [1]–[3] and has been widely utilized in applications such as resourceThe associate editor coordinating the review of this manuscript and approving it for publication was X

  • The experimental results show that the proposed interpolation method improves both the accuracy and efficiency of the faulted geological surface model compared to the ORDINARY KRIGING (OK), Hermite RBF (HRBF), and multiscale CSRBF methods

  • 3) IMPLEMENT INTERPOLATION The TRIANGULATED IRREGULAR NETWORK (TIN)-constrained OK method is implemented in this step, as detailed in Section 3.3, with an input of the extracted geological sample points and computed fault horizontal cutoff lines and an output of a set of points located on the geological surface

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Summary

Introduction

Three-dimensional (3D) structural modeling helps geologists understand the physical world [1]–[3] and has been widely utilized in applications such as resourceThe associate editor coordinating the review of this manuscript and approving it for publication was X. The constrained Delaunay triangulations (CDT) algorithm [35] is performed to construct a TIN using the sample points and fault cutoff lines to constrain its neighborhood search process for locating neighbor points used in the interpolation.

Results
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