@article{10272/8207,
year = {2008},
url = {http://hdl.handle.net/10272/8207},
abstract = {Geological map of Virgen de la Peña rock massif has established that there are three sets of geological
discontinuities in the rock mass: a) stratification set strikes NW-SE and dips more 70º NE; b) faults set
strikes NE-SW and has gently dips and c) joints set strike NE-SW showing steeply dips. Cubical or tabulate
blocks are formed by three intersecting discontinuity sets. The analysis of stability of rock massif illustrates
the mechanics of failure involve the block toppling and sliding. The index Rock Mass Rating (RMR, Bieniawski,
1989) is obtained},
keywords = {Rock massif},
keywords = {Block toppling},
keywords = {Plane failure},
keywords = {Engineering geology},
keywords = {Puebla de Guzmán Anticline},
title = {Análisis de los tipos de intestabilidades del macizo rocoso de La Virgen de la Peña (Huelva, España)},
title = {Analysis of the instabilities types in the Rock Massif of Virgen de la Peña (Huelva, Spain)},
author = {Alonso Chaves, Francisco Manuel and García Navarro, Encarnación and Camacho Cerro, Manuel Alejandro and Mantero Romero, Elena María},
}