1. Almeida, E., Pous, J., Monteiro, Santos F., Fonseca, P., Marcuello, A., Queralt, P., Nolasco, R., and Mendes-Victor, L., Electromagnetic imaging of a compressional tectonic in SW Iberia, Geophys. Res. Lett., 2001, vol. 28, 439–442. https://doi.org/10.1029/2000GL012037
2. Anderson, T.B., Kink bands and related geological structures, Nature, 1964, vol. 202, pp. 272–274. https://doi.org/10.1038/2101249a0
3. Andrade, A. S., Remarques sur le chemisme des gabros d’Odivelas (Massif de Beja), Mem. Not. Publ. Mus. Lab. Mineral. Geol. Univ. Coimbra, 1976, vol. 81, pp. 75–84.
4. Andrade, A.S., Sur l’âge des orthogneiss d’Alcáçovas (Alentejo)—et des filons (basiques et acides que les recounpent, Mem. Not. Mus. Lab. Mineral. Geol., Univ. Coimbra, 1974, vol. 78, pp. 29–36.
5. Apalategui, O., Eguiluz, L., and Quesada, C., Ossa Morena Zone, structure, Pre-Mesozoic Geology of Iberia, R.D. Dallmeyer and E. Martínez-García, Eds., Springer–Verlag, 1990, vol. 2, 80–219.