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http://hdl.handle.net/2183/5829 Tectónica cuaternaria en el área de Almunia (provincia de Zaragoza)
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Gutiérrez Elorza, M.
Simón Gómez, J. L.
Soriano Jiménez, M. A.
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Cadernos do Laboratorio Xeolóxico de Laxe, 1983, 5: 421-428 ISBN: 84-7492-198-8
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Abstract
[Resumen] Los depósitos pliocuaternarios de la Almunia aparecen basculados contra las sierras ibéricas como consecuencia de la probable reactivación de una falla de borde NW-SE. Las deformaciones parecen prolongarse durante el Pleistoceno antíguo
[Abstract] Pliocuaternary deposits of La Almunia are –tilted to Iberian Range by probable reactivation of a NW-SE fault on the boundary with the Ebro Bassin. The deformations are probably prolongated during Early Pleistocene
[Abstract] Pliocuaternary deposits of La Almunia are –tilted to Iberian Range by probable reactivation of a NW-SE fault on the boundary with the Ebro Bassin. The deformations are probably prolongated during Early Pleistocene