Section-constrained local geological interface dynamic updating method based on the HRBF surface. (February 2018)

• Record Type: Journal Article
• Authors: Guo, Jiateng; Wu, Lixin; Zhou, Wenhui; Li, Chaoling; Li, Fengdan
• Is Part Of: Journal of structural geology. Volume 107(2018)
• Page Start: 64
• Page End: 72
• Publication Date: 2018-02
• Subjects: 3D regional geological modelling -- Hermite radial basis function -- Section constraint -- Dynamic model modification; Geology, Structural -- Periodicals; Géomorphologie structurale -- Périodiques; Geology, Structural; Periodicals; 551.805
• DOI: 10.1016/j.jsg.2017.11.017
• Languages: English
• ISSNs: 0191-8141

Abstract

Abstract: Boundaries, attitudes and sections are the most common data acquired from regional field geological surveys, and they are used for three-dimensional (3D) geological modelling. However, constructing topologically consistent 3D geological models from rapid and automatic regional modelling with convenient local modifications remains unresolved. In previous works, the Hermite radial basis function (HRBF) surface was introduced for the simulation of geological interfaces from geological boundaries and attitudes, which allows 3D geological models to be automatically extracted from the modelling area by the interfaces. However, the reasonability and accuracy of non-supervised subsurface modelling is limited without further modifications generated through explanations and analyses performed by geology experts. In this paper, we provide flexible and convenient manual interactive manipulation tools for geologists to sketch constraint lines, and these tools may help geologists transform and apply their expert knowledge to the models. In the modified modelling workflow, the geological sections were treated as auxiliary constraints to construct more reasonable 3D geological models. The geometric characteristics of section lines were abstracted to coordinates and normal vectors, and along with the transformed coordinates and vectors from boundaries and attitudes, these characteristics were adopted to co-calculate the implicit geological surface function parameters of the HRBF equations and form constrained geological interfaces from topographic (boundaries and attitudes) and subsurface data (sketched sections). Based on this new modelling method, a prototype system was developed, in which the section lines could be imported from databases or interactively sketched, and the models could be immediately updated after the new constraints were added. Experimental comparisons showed that all boundary, attitude and section data are well represented in the constrained models, which are consistent with expert explanations and help improve the quality of the models. Highlights: Geological sections were treated as auxiliary constraints in the rapid and automatic 3D geological modeling workflow. Convenient manual interactive manipulation tools were provided for geologists to sketch constraint section lines. Geologists' expert knowledge could be added to the initial models by sketching section lines for dynamically local updating.