Abstract
Using a technique with computational methods, the organization of the topographical linearments, the geological fissures and others as the structural discontinuities of the earth were simulated on the new morphological models.
It has developed a new net model with geometrical polygons on the Voronoi regions as Finite Element Model. After the results, the characteristics of their statistical parameters show good answers and adaptations about the simulations as the linearments on the topographical surface, crack-lines on the rock-bodies and etc. Especially, presented patterns of fractal slipped lines had in native. On this studies as the plane problem, the new experiences produced several good informations for the way to approach the geological structures on the earth.
