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Our burial model reveals that Mesozoic extension occurred during three main phases, each comprising distinct subsidence pulses separated by short\u2010lived periods of crustal uplift. The importance of the three phases varies across discrete sectors of the margin, each one revealing similar depositional architectures and associated tectonic systems tracts: 1) the Rift Initiation phase, characterized by incipient subsidence and overall aggradation\/progradation over a basal unconformity, 2) the Rift Climax phase, which marks maxima of tectonic subsidence and is characterized by retrogradation\u2010progradation, and 3) the Late Rift phase, recording the progradational infill of the basin and the effects of eustasy. The Rift Initiation systems tracts comprise Sinemurian and late Callovian\u2010early Oxfordian strata. Marine units in the Pliensbachian and Late Oxfordian\u2010Kimmeridgian represent the Rift Climax phase, a period marked by the development of Maximum Flooding Surfaces. Late Rift deposits were identified in the Rhaetian\u2010Hettangian, Toarcian\u2010Bathonian and Kimmeridgian\u2010Berriasian. The results of this work are important to the economic exploration of deep\u2010offshore rift basins, as they reveal that sequence stratigraphy can be used to predict sedimentary facies distribution in more distal segments of such basins. Significantly, this work recognizes that multiple tectonic\u2010stratigraphic (rift) cycles can occur on deep\u2010offshore rift basins, from the onset of rift\u2010related extension until continental break\u2010up, a character that contrast to what is known from deep\u2010sea drilling data from the distal margin of Northwest Iberia.<\/jats:p>","DOI":"10.1029\/2011tc003001","type":"journal-article","created":{"date-parts":[[2012,5,25]],"date-time":"2012-05-25T07:58:06Z","timestamp":1337932686000},"source":"Crossref","is-referenced-by-count":46,"title":["Tectono\u2010stratigraphic signature of multiphased rifting on divergent margins (deep\u2010offshore southwest Iberia, North Atlantic)"],"prefix":"10.1029","volume":"31","author":[{"given":"Ricardo","family":"Pereira","sequence":"first","affiliation":[]},{"given":"Tiago M.","family":"Alves","sequence":"additional","affiliation":[]}],"member":"13","published-online":{"date-parts":[[2012,7,4]]},"reference":[{"key":"e_1_2_9_2_1","doi-asserted-by":"publisher","DOI":"10.1016\/j.tecto.2008.03.002"},{"key":"e_1_2_9_3_1","doi-asserted-by":"publisher","DOI":"10.1016\/S0025\u20103227(02)00683\u20107"},{"key":"e_1_2_9_4_1","doi-asserted-by":"publisher","DOI":"10.1016\/S0037\u20100738(03)00155\u20106"},{"key":"e_1_2_9_5_1","doi-asserted-by":"publisher","DOI":"10.1306\/08110504138"},{"key":"e_1_2_9_6_1","doi-asserted-by":"publisher","DOI":"10.1029\/2008TC002337"},{"key":"e_1_2_9_7_1","doi-asserted-by":"publisher","DOI":"10.1046\/j.1365\u20103091.2002.00501.x"},{"key":"e_1_2_9_8_1","unstructured":"Azer\u00eado A. 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