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The Azuaga Fault bounds a Devonian suture zone known as Central Unit. This fault is a steeply NE\u2010dipping, Variscan strike\u2010slip fault with left\u2010lateral and reverse oblique slip components formed during sinistral transpression in the Pennsylvanian. Motion along this fault was coeval with folding and fabric development in both its hanging wall and footwall, and also with the Matachel Fault. Tectonic flow associated with the Azuaga Fault shows high\u2010vorticity, explaining the exhumation of a flat\u2010lying Devonian suture zone via WNW\u2010plunging extrusion from the upper\u2010middle crust under inclined triclinic transpression during ENE\u2010WSW convergence. The exposed basal contact of the Central Unit is not the root zone of a Variscan suture zone, but instead is a NE\u2010dipping breaching fault that cuts across the suture zone that is contiguous to the SW under the upper section of the footwall. The peri\u2010Gondwanan terrane between the Central Unit and the South\u2010Portuguese Zone of the Iberian Massif (most of the Ossa\u2010Morena Zone) is underlain by a Devonian suture, implying it is a continental allochthon. Variscan suture zones in Europe are affected by strike\u2010slip faults. In our case, this pattern implies the location of suture zone exposures and location of its root are different. Suture zones and strike\u2010slip faults are common in orogens and analysis of their relationships may lead to relocation of suture zone roots and re\u2010thinking of upper and lower plates.<\/jats:p>","DOI":"10.1029\/2021tc006791","type":"journal-article","created":{"date-parts":[[2021,5,24]],"date-time":"2021-05-24T12:23:22Z","timestamp":1621859002000},"update-policy":"https:\/\/doi.org\/10.1002\/crossmark_policy","source":"Crossref","is-referenced-by-count":9,"title":["On the Rootless Nature of a Devonian Suture in SW Iberia (Ossa\u2010Morena Complex, Variscan Orogen): Geometry and Kinematics of the Azuaga Fault"],"prefix":"10.1029","volume":"40","author":[{"ORCID":"https:\/\/orcid.org\/0000-0002-0379-7970","authenticated-orcid":false,"given":"Rub\u00e9n D\u00edez","family":"Fern\u00e1ndez","sequence":"first","affiliation":[{"name":"Instituto Geol\u00f3gico y Minero de Espa\u00f1a (IGME) CSIC  Madrid Spain"}]},{"ORCID":"https:\/\/orcid.org\/0000-0001-5135-7972","authenticated-orcid":false,"given":"Carlos","family":"Fern\u00e1ndez","sequence":"additional","affiliation":[{"name":"Departamento de Ciencias de la Tierra Universidad de Huelva Campus de El Carmen  Huelva Spain"},{"name":"Now at Departamento de Geodin\u00e1mica, Estratigraf\u00eda y Paleontolog\u00eda Universidad Complutense  Madrid Spain"}]},{"given":"Ricardo","family":"Arenas","sequence":"additional","affiliation":[{"name":"Departamento de Petrolog\u00eda y Geoqu\u00edmica e Instituto de Geociencias (UCM, CSIC) Universidad Complutense  Madrid Spain"}]},{"given":"Irene","family":"Novo\u2010Fern\u00e1ndez","sequence":"additional","affiliation":[{"name":"Departamento de Petrolog\u00eda y Geoqu\u00edmica e Instituto de Geociencias (UCM, CSIC) Universidad Complutense  Madrid Spain"}]}],"member":"13","published-online":{"date-parts":[[2021,6,17]]},"reference":[{"key":"e_1_2_10_2_1","first-page":"430","volume-title":"Cinem\u00e1tica y mecanismos de la deformaci\u00f3n en r\u00e9gimen de transpresi\u00f3n: Evoluci\u00f3n estructural y metam\u00f3rfica de la zona de Cizalla d\u00factil de Badajoz\u2010C\u00f3rdoba, PhD thesis","author":"\u00c1balos B.","year":"1990"},{"key":"e_1_2_10_3_1","first-page":"229","article-title":"Deformaci\u00f3n transpresiva carbon\u00edfera en la Zona de Cizalla de Badajoz\u2010C\u00f3rdoba (Macizo Ib\u00e9rico meridional)","volume":"4","author":"Abalos B.","year":"1991","journal-title":"Revista de la Sociedad Geologica de Espana"},{"key":"e_1_2_10_4_1","first-page":"617","article-title":"Evoluci\u00f3n tectono\u2010metam\u00f3rfica del Corredor Blastomilon\u00edtico de Badajoz\u2010C\u00f3rdoba. 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