Volume 42 Issue 5
Sep.  2023
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Wang Quan, Zou Yanhong. Three-dimensional geological implicit surface reconstruction based on intermediate contour morphological interpolation[J]. Bulletin of Geological Science and Technology, 2023, 42(5): 293-300. doi: 10.19509/j.cnki.dzkq.tb20220003
Citation: Wang Quan, Zou Yanhong. Three-dimensional geological implicit surface reconstruction based on intermediate contour morphological interpolation[J]. Bulletin of Geological Science and Technology, 2023, 42(5): 293-300. doi: 10.19509/j.cnki.dzkq.tb20220003

Three-dimensional geological implicit surface reconstruction based on intermediate contour morphological interpolation

doi: 10.19509/j.cnki.dzkq.tb20220003
  • Received Date: 04 Jan 2022
  • Accepted Date: 22 Feb 2022
  • Rev Recd Date: 21 Feb 2022
  • Objective

    In three-dimensional morphological reconstruction of complex geological surfaces, the sparse geological section data cannot meet the modelling requirements. To overcome it, in this paper, we propose a 3D geological implicit surface reconstruction method based on intermediate contour morphological interpolation at the maximum similarity.

    Methods

    Firstly, a fuzzy vertex correspondence algorithm was used to generate multiple contour vertex mapping sets of two adjacent contours of the same geological body. Then, the contour similarity coefficient was obtained by calculating the similarity degree of matching points, and the best contour vertex matching map is established based on maximum similarity matching principle; Finally, through intermediate gradient interpolation, the result is used as a morphological constraint to participate in surface reconstruction with radial basis functions (RBFs).

    Results

    Taking the practical geological section as an example, we constructed the three-dimensional geological implicit model based on morphological interpolation.

    Conclusion

    Results show that the proposed method can not only realize reasonable intermediate morphology transition between two adjacent sparse contours, but also overcome the phenomenon of excessively smooth or discontinuous surfaces caused by sparse data during implicit surface reconstruction, providing a new basis for complex geological surface reconstruction based on implicit functions.

     

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