Abstract
The mechanical and hydrological behaviour of fractured media depends on the morphology of single fractures. Geostatistics enables modelling of the topography of both fracture surfaces and the aperture. The small-scale variations of a fracture surface depend on the angularity of individual grain facets and are modelled by means of a combined variography of the elevation and its first derivatives. The topography of the two fracture sides and the void height are studied simultaneously and consistently with specific tools, such as cross-covariance and the translatogram.
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© 1993 Kluwer Academic Publishers
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Chilès, JP., Gentier, S. (1993). Geostatistical Modelling of a Single Fracture. In: Soares, A. (eds) Geostatistics Tróia ’92. Quantitative Geology and Geostatistics, vol 5. Springer, Dordrecht. https://doi.org/10.1007/978-94-011-1739-5_9
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DOI: https://doi.org/10.1007/978-94-011-1739-5_9
Publisher Name: Springer, Dordrecht
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