@article{10272/10248,
year = {1997},
url = {http://hdl.handle.net/10272/10248},
abstract = {Thire are three regional joint sets in the central Ebro, basin. The southern part is. dominated by a primary N-S striking joint set and a secondary E-W set. In the nortnern part, the primary joint set strikes NW-SE Detailed outcrop observations where the three sets do coexist suggest that the E-W set is the result of stress perturbation originated by the previous N-S set over the extensionat NE-SW stress field responsible for the development of the NW-SE joints in the northern area},
publisher = {Sociedad Geológica de España},
title = {Las diaclàsas E-W y NW-SE fen el sector central de la Cuenca del Ebro. Relation con el campo de esfuerzos Neógeno},
title = {The E-W and NW-Sh trending joint sets in the Central Ebro Basin (Spain). Relationship with the neogene stress field},
author = {Arlegui, L. E. and Simón Gómez, José Luis},
}