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Spatial Distribution,Scaling and Self-similar Behavior of Fracture Arrays in the Los Planes Fault,Baja California Sur,Mexico
Authors:Email author" target="_blank">A F?Nieto-SamaniegoEmail author  S A?Alaniz-Alvarez  G?Tolson  K?Oleschko  G?Korvin  S S?Xu  J A?Pérez-Venzor
Institution:(1) Universidad Nacional Autónoma de México, Centro de Geociencias. Apartado postal 1-742, Querétaro, Qro., 76001, Mexico;(2) Instituto de Geología, Universidad Nacional Autónoma de México, Ciudad Universitaria, Apartado postal 70-296, D. F., 04510, México, Mexico;(3) King Fahd University, Mail Box 1157, Dhahran, 31261, Saudi Arabia;(4) Departamento de Geología Marina, Universidad Autónoma de Baja California Sur, Apartado postal 19-B, La Paz, Baja California Sur, 23080, Mexico
Abstract:We present a case of detailed analysis of fracture arrays spanning four orders of magnitude in length; all of them measured at a single natural site by acquiring images at progressively larger scales. There is a high dispersion of cumulative-length exponents, box dimensions and fracture densities. However, the fractal analysis supports the fractal nature of fracture arrays. Our data indicate the existence of an upper limit for the density parameters, as similarly reported by other authors. We prove that box dimension is in inverse relation with fracture concentration and in direct relation with fracture density. These relations are also observed in our data and additionally there is an upper limit for the box dimensions. We interpret the dispersion in our results as more fundamental than methodological problems. It represents a truncation in the complete evolution of the fracture systems because in natural cases strain initiates overprinting of previous fracture arrays. Considering that larger fractures accommodate strain more efficiently than small fractures, the generation of small fractures is inhibited in the presence of pre-existing larger fractures. Maximum values of fracture density prevent accommodating an excess of strain in a single or restricted range of scales; we claim this condition produces migration of fracturing to larger scales originating fracture scaling.
Keywords:Fracture arrays  fracture density  self-similarity  scaling-law  fractal analysis
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