Fractal geometry and seismicity in the Mexican subduction zone
By means of the box counting method we calculate the fractal dimension D of the distribution of faults, fractures and lineaments in a region of the southern Mexican Pacific coast. The results suggest that in the spatial sense the b-value of the Gutenberg-Richter law and the fractal dimension are pos...
| Autores: | , , , , |
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| Tipo de recurso: | artículo |
| Estado: | Versión publicada |
| Fecha de publicación: | 1998 |
| País: | México |
| Institución: | UNIVERSIDAD NACIONAL AUTÓNOMA DE MÉXICO |
| Repositorio: | Geofísica Internacional |
| Idioma: | español |
| OAI Identifier: | oai:revistagi.geofisica.unam.mx:article/591 |
| Acceso en línea: | http://revistagi.geofisica.unam.mx/index.php/RGI/article/view/591 |
| Access Level: | acceso abierto |
| Palabra clave: | Geometría fractal sismos Guerrero México Fractal geometry earthquakes Mexico |
| Sumario: | By means of the box counting method we calculate the fractal dimension D of the distribution of faults, fractures and lineaments in a region of the southern Mexican Pacific coast. The results suggest that in the spatial sense the b-value of the Gutenberg-Richter law and the fractal dimension are positively correlated. We also suggest that D depends on the depth of the seismogenic zone. |
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