he geometrical description of fault patterns in a given rock mass can be made through an estimation of three sets of quantitative parameters
CITATION STYLE
Villemin, T., Angelier, J., & Sunwoo, C. (1995). Fractal Distribution of Fault Length and Offsets: Implications of Brittle Deformation Evaluation—The Lorraine Coal Basin. In Fractals in the Earth Sciences (pp. 205–226). Springer US. https://doi.org/10.1007/978-1-4899-1397-5_10
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