一种面向三维地质剖面数据的形体表面重构算法
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摘要
三维表面形体重构方法大多是基于二维平行轮廓线的,这种基于二维平行轮廓线的方法已广泛应用于医学影像、地学建模等领域。但是,在地学建模领域,利用地质剖面进行三维表面重建时,难免会有既不平行也不交叉的剖面出现。针对这种情况,该文基于最短对角线法的基本思路,提出了一种面向地质剖面的三维空间轮廓线表面形体重构方法。该方法从平行剖面拓展到任意排列的剖面,在实现三维空间相关运算的基础上,通过基于均匀插值的三维非凸变换方法对原算法进行了改进,既适用于平行和非平行地质剖面的三维形体重构,同时,又能处理真实地质剖面可能出现的复杂情形,譬如轮廓线不对中、轮廓线上点分布不均匀、轮廓线非凸等。最后,利用矿区真实地质剖面实现了形体重构,验证了本算法的适应性和健壮性;同时,通过与三维建模软件GOCAD进行比较,验证了本算法的先进性和实用性。
From the existing research of 3D-reconstruction we can find: most reconstruction algorithms are based on 2D planar contours and are widely applied in medical images and geological modeling. But in the area of Geoscience, sometimes contours which are neither planar nor cross can emerge. Inspired by the shortest diagonal method, in this paper, a 3D geological surface reconstruction method tailored for geological profiles is presented, which is expanded from 2D to 3D space, not only allows the reconstruction from parallel geological cross-sections, but also achieves good performance when given arbitrary cross-sections. In this method, uniform interpolation is applied to passivate the sharp edges while maintaining the accuracy, and a new non-convex contours transformation algorithm is proposed to avoid the crossings in which commonly-used recursive operation is discarded and the complexity of algorithm is correspondingly reduced. This method is more adaptive and robust to handle complex scenarios existing in the geological sections such as non-aligned contours, non-convex contours and contours of uneven vertices, which is validated with the surface reconstruction test with practical geological profile data. The comparison with the commercial 3D modeling software GOCAD further shows good progressiveness and practicability of the method.
引文
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