
handle: 10272/16406
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
Huesca, Joints, Stress field, Deflection, Alpine tectonics, Ebro basin
Huesca, Joints, Stress field, Deflection, Alpine tectonics, Ebro basin
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