@article{10272/16406,
year = {1992},
url = {http://hdl.handle.net/10272/16406},
abstract = {Neotectonic joints in the Ebro basin strike uniformly NNW-SSE, perpendicular or nearperpendicular to the direction of <33 in the moment it developed. Within the Sierra de Sigena there are joints with anomalous strikes. They show a vertical evolution becoming more similar to the regional fracture pattern as higher in the slope they appair. In the middle portion of the slope this set coexists with the regional-striking joints We interpret this joint distribution as a consequence of stress deflection caused by major faults in the basament, which shows possible attenuation upwards},
publisher = {Sociedad Geológica de España},
keywords = {Joints},
keywords = {Stress field},
keywords = {Deflection},
keywords = {Huesca},
keywords = {Ebro basin},
keywords = {Alpine tectonics},
title = {Variación del patrón de diaclasas a lo largo de la serie neógena de la Sierra de Sigena (Huesca): Posible relación con el campo de esfuerzos y su perturbación},
title = {Variation in the joint pattern along the neogene series of the Sierra de Sigena (Huesca): Possible relationships with the stress Field and its deflection},
author = {Arlegui, L. E.},
}