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The evidence in this paper indicates distinct crustal architectures for NW Iberia (lower-plate) and SW Iberia (upper-plate), as shown by (1) the different geometries of the rotated tilt-blocks across thinned continental crust, (2) the distinct dips of deep crustal detachments and (3) the presence of first-order strike-slip zones bounding different crustal segments. We demonstrate that a switch in the dip direction of the crustal detachment is accomplished by accommodating persistent transcurrent deformation along first-order transfer zones and associated uplifted hinges, both of which accommodated synrift displacement and post-rift margin inversion. This alternating architecture explains why recurrent magmatism is conspicuously located on the upper-plate margin, which we consider to have favoured, in discrete pulses, the emplacement of magma. Finally, the crustal detachment underlying the upper-plate is interpreted to have been reactivated since the Eocene as the weak zone accommodating ocean\u2013continent convergence and the putative onset of margin subduction.<\/jats:p>\n          <jats:p content-type=\"supplementary-material\">\n            <jats:bold>Supplementary material:<\/jats:bold>\n            Summary of the three main magmatic events on the onshore and offshore West Iberia and their associated occurrences, location and magmatism type, in relation with the syn- to post-rift evolution of the margin are available at\n            <jats:ext-link xmlns:xlink=\"http:\/\/www.w3.org\/1999\/xlink\" ext-link-type=\"uri\" xlink:href=\"https:\/\/doi.org\/10.6084\/m9.figshare.c.3591209\">https:\/\/doi.org\/10.6084\/m9.figshare.c.3591209<\/jats:ext-link>\n          <\/jats:p>","DOI":"10.1144\/jgs2016-050","type":"journal-article","created":{"date-parts":[[2016,12,23]],"date-time":"2016-12-23T07:43:28Z","timestamp":1482479008000},"page":"522-540","update-policy":"https:\/\/doi.org\/10.1144\/crossmark-policy","source":"Crossref","is-referenced-by-count":31,"title":["Alternating crustal architecture in West Iberia: a review of its significance in the context of NE Atlantic rifting"],"prefix":"10.1144","volume":"174","author":[{"given":"Ricardo","family":"Pereira","sequence":"first","affiliation":[{"name":"Partex Oil and Gas, Rua Ivone Silva, 6, 1st floor, 1050-124, Lisbon, Portugal"},{"name":"Instituto Dom Luiz, Faculdade de Ci\u00eancias da Universidade de Lisboa Campo Grande, Edif\u00edcio C1, Piso 1, 1749-016 Lisbon, Portugal"}]},{"given":"Tiago M.","family":"Alves","sequence":"additional","affiliation":[{"name":"3D Seismic Lab, School of Earth and Ocean Sciences, Cardiff University, Main Building, Park Place, Cardiff CF10 3AT, UK"}]},{"given":"Jo\u00e3o","family":"Mata","sequence":"additional","affiliation":[{"name":"Instituto Dom Luiz, Faculdade de Ci\u00eancias da Universidade de Lisboa Campo Grande, Edif\u00edcio C1, Piso 1, 1749-016 Lisbon, Portugal"}]}],"member":"1881","published-online":{"date-parts":[[2016,12,22]]},"reference":[{"key":"e_1_3_2_2_1","doi-asserted-by":"publisher","DOI":"10.1016\/j.tecto.2008.03.002"},{"key":"e_1_3_2_3_1","first-page":"243","article-title":"Tertiary evolution of the S\u00e3o Vicente and Set\u00fabal submarine canyons, Southwest Portugal: insights from seismic stratigraphy","volume":"14","author":"Alves T.M.","year":"2000","unstructured":"Alves, T.M., Gawthorpe, R.L., Hunt, D. & Monteiro, J.H. 2000. 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