Three-Dimensional Modelling of Geological Surfaces Using Generalized Interpolation with Radial Basis Functions

被引:138
作者
Hillier, Michael J. [1 ]
Schetselaar, Ernst M. [1 ]
de Kemp, Eric A. [1 ]
Perron, Gervais [2 ]
机构
[1] Geol Survey Canada, Ottawa, ON K1A 0E9, Canada
[2] Mira Geosci Ltd, Montreal, PQ H3Z 2M9, Canada
关键词
Three-dimensional geomodelling; Structural geology; Implicit modelling; Radial basis functions; Generalized interpolation; POSITIVE-DEFINITE FUNCTIONS; FIELD INTERPOLATION; 3D; RESTORATION; EQUATIONS; INVERSION; FRAMEWORK; SPLINES; FOLDS;
D O I
10.1007/s11004-014-9540-3
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
A generalized interpolation framework using radial basis functions (RBF) is presented that implicitly models three-dimensional continuous geological surfaces from scattered multivariate structural data. Generalized interpolants can use multiple types of independent geological constraints by deriving for each, linearly independent functionals. This framework does not suffer from the limitations of previous RBF approaches developed for geological surface modelling that requires additional offset points to ensure uniqueness of the interpolant. A particularly useful application of generalized interpolants is that they allow augmenting on-contact constraints with gradient constraints as defined by strike-dip data with assigned polarity. This interpolation problem yields a linear system that is analogous in form to the previously developed potential field implicit interpolation method based on co-kriging of contact increments using parametric isotropic covariance functions. The general form of the mathematical framework presented herein allows us to further expand on solutions by: (1) including stratigraphic data from above and below the target surface as inequality constraints (2) modelling anisotropy by data-driven eigen analysis of gradient constraints and (3) incorporating additional constraints by adding linear functionals to the system, such as fold axis constraints. Case studies are presented that demonstrate the advantages and general performance of the surface modelling method in sparse data environments where the contacts that constrain geological surfaces are rarely exposed but structural and off-contact stratigraphic data can be plentiful.
引用
收藏
页码:931 / 953
页数:23
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