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In the 1970s and 1980s, most researchers considered this margin typical of a non-volcanic passive margin: it is characterized by a striking succession of tilted blocks beneath which occurs the S reflector and the continent\u2013ocean boundary is abrupt. This paper examines the Armorican segment and is based on a study of all early seismic profiles together with new multichannel reflection and refraction seismic data (Norgasis cruise). An important result is the discovery of a 80 km wide ocean\u2013continent transition zone that coincides with the Armorican Basin (a deep sedimentary basin). It is characterized by a high-velocity lower-crustal layer (7.4\u20137.5 km s\n            <jats:sup>\u22121<\/jats:sup>\n            ) overlain by sediments. The other results are: (1) the main crustal thinning occurs exclusively under the narrow continental slope; (2) the tilted blocks and the S reflector are observed only at the base of the continental slope in the narrow domain called the \u2018neck area\u2019; (3) the North Biscay Ridge is a large oceanic plateau present only off the NW Armorican margin rather than a long ridge elongated off the whole North Biscay margin.\n          <\/jats:p>","DOI":"10.1144\/0016-764901-103","type":"journal-article","created":{"date-parts":[[2007,12,21]],"date-time":"2007-12-21T18:24:55Z","timestamp":1198261495000},"page":"99-116","update-policy":"https:\/\/doi.org\/10.1144\/crossmark-policy","source":"Crossref","is-referenced-by-count":82,"title":["Deep structure of the Armorican Basin (Bay of Biscay): a review of Norgasis seismic reflection and refraction data"],"prefix":"10.1144","volume":"160","author":[{"given":"I.","family":"Thinon","sequence":"first","affiliation":[{"name":"1BRGM-CDG\/MA, 3 avenue Claude Guillemin, BP 6009, 45060 Orle\u0301ans cedex 2, France (e-mail: i.thinon@brgm.fr)"}]},{"given":"L.","family":"Matias","sequence":"additional","affiliation":[{"name":"2Centro de Geofisica, Rua da escola Politecnica 58, 1200 Lisbon, Portugal"}]},{"given":"J.P.","family":"RE\u0301hault","sequence":"additional","affiliation":[{"name":"3IUEM-UBO, UMR6538 du CNRS, Place Nicolas Copernic 29280 Plouzane\u0301, France"}]},{"given":"A.","family":"Hirn","sequence":"additional","affiliation":[{"name":"4De\u0301partement de Sismologie, UA195 CNRS, IPG, 4 place Jussieu, 75252 Paris 05, France"}]},{"given":"L.","family":"Fidalgo-GonzA\u0301lez","sequence":"additional","affiliation":[{"name":"3IUEM-UBO, UMR6538 du CNRS, Place Nicolas Copernic 29280 Plouzane\u0301, France"},{"name":"5IFREMER, DRO-GM, BP 70, Place Nicolas Copernic 29280 Plouzane\u0301, France"}]},{"given":"F.","family":"Avedik","sequence":"additional","affiliation":[{"name":"3IUEM-UBO, UMR6538 du CNRS, Place Nicolas Copernic 29280 Plouzane\u0301, France"},{"name":"5IFREMER, DRO-GM, BP 70, Place Nicolas Copernic 29280 Plouzane\u0301, France"}]}],"member":"1881","published-online":{"date-parts":[[2022,6,6]]},"reference":[{"key":"e_1_3_2_1_1","doi-asserted-by":"crossref","unstructured":"Avedik F. 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