{"status":"ok","message-type":"work","message-version":"1.0.0","message":{"indexed":{"date-parts":[[2026,2,25]],"date-time":"2026-02-25T01:26:08Z","timestamp":1771982768147,"version":"3.50.1"},"reference-count":23,"publisher":"American Geophysical Union (AGU)","issue":"1","license":[{"start":{"date-parts":[[2022,1,20]],"date-time":"2022-01-20T00:00:00Z","timestamp":1642636800000},"content-version":"vor","delay-in-days":19,"URL":"http:\/\/onlinelibrary.wiley.com\/termsAndConditions#vor"}],"funder":[{"DOI":"10.13039\/501100011033","name":"Agencia Estatal de Investigaci\u00f3n","doi-asserted-by":"publisher","award":["PID2020\u2010112489GB\u2010C22"],"award-info":[{"award-number":["PID2020\u2010112489GB\u2010C22"]}],"id":[{"id":"10.13039\/501100011033","id-type":"DOI","asserted-by":"publisher"}]},{"DOI":"10.13039\/501100011033","name":"Agencia Estatal de Investigaci\u00f3n","doi-asserted-by":"publisher","award":["PID2020\u2010112489GB\u2010C21"],"award-info":[{"award-number":["PID2020\u2010112489GB\u2010C21"]}],"id":[{"id":"10.13039\/501100011033","id-type":"DOI","asserted-by":"publisher"}]}],"content-domain":{"domain":["agupubs.onlinelibrary.wiley.com"],"crossmark-restriction":true},"short-container-title":["Tectonics"],"published-print":{"date-parts":[[2022,1]]},"abstract":"<jats:title>Abstract<\/jats:title><jats:p>Geological mapping, structural data, and analytical modeling by D\u00edez Fern\u00e1ndez et\u00a0al. (2021),<jats:ext-link xmlns:xlink=\"http:\/\/www.w3.org\/1999\/xlink\" xlink:href=\"https:\/\/doi.org\/10.1029\/2021tc006791\">https:\/\/doi.org\/10.1029\/2021tc006791<\/jats:ext-link>supported that the Central Unit belonged to a rootless Devonian suture zone contiguous to the SW of its exposure and under the upper section of the footwall to the Azuaga Fault. Late exhumation of the Central Unit was via extrusion from the upper\u2010middle crust under inclined triclinic sinistral transpression, which favored upright folding of the suture zone. Azor and coworkers argue that the upright folds that affect the Central Unit are local, despite geological maps and structural data demonstrate they are km\u2010scale and occur all across the Central Unit. Besides ignoring structural data regarding the kinematics of the Azuaga Fault, Azor et\u00a0al. (2022),<jats:ext-link xmlns:xlink=\"http:\/\/www.w3.org\/1999\/xlink\" xlink:href=\"https:\/\/doi.org\/10.1029\/2021TC006982\">https:\/\/doi.org\/10.1029\/2021TC006982<\/jats:ext-link>fail to recognize the net upthrown movement of the NE side of the Azuaga Fault, as the Central Unit in that side is juxtaposed against syn\u2010orogenic strata that rest unconformably onto other metamorphic units in the SW side of the fault. Seismic data that image the Central Unit as a NE\u2010dipping rock package is used as an argument against the proposal by D\u00edez Fern\u00e1ndez et\u00a0al. (2021),<jats:ext-link xmlns:xlink=\"http:\/\/www.w3.org\/1999\/xlink\" xlink:href=\"https:\/\/doi.org\/10.1029\/2021tc006791\">https:\/\/doi.org\/10.1029\/2021tc006791<\/jats:ext-link>. However, the section of the Central Unit those data account for, are from a different part of the Central Unit, the real dip of some structures in the seismic image is not properly interpreted, and the model by D\u00edez Fern\u00e1ndez et\u00a0al. (2021),<jats:ext-link xmlns:xlink=\"http:\/\/www.w3.org\/1999\/xlink\" xlink:href=\"https:\/\/doi.org\/10.1029\/2021tc006791\">https:\/\/doi.org\/10.1029\/2021tc006791<\/jats:ext-link>is compatible with a Central Unit that also dips to the NE. Overall, the model proposed by D\u00edez Fern\u00e1ndez et\u00a0al. (2021),<jats:ext-link xmlns:xlink=\"http:\/\/www.w3.org\/1999\/xlink\" xlink:href=\"https:\/\/doi.org\/10.1029\/2021tc006791\">https:\/\/doi.org\/10.1029\/2021tc006791<\/jats:ext-link>remains valid.<\/jats:p>","DOI":"10.1029\/2021tc007154","type":"journal-article","created":{"date-parts":[[2022,1,11]],"date-time":"2022-01-11T19:48:41Z","timestamp":1641930521000},"update-policy":"https:\/\/doi.org\/10.1002\/crossmark_policy","source":"Crossref","is-referenced-by-count":3,"title":["Reply to Comment by Azor et al. on \u201cOn the Rootless Nature of a Devonian Suture in SW Iberia (Ossa\u2010Morena Complex, Variscan Orogen): Geometry and Kinematics of the Azuaga Fault\u201d"],"prefix":"10.1029","volume":"41","author":[{"ORCID":"https:\/\/orcid.org\/0000-0002-0379-7970","authenticated-orcid":false,"given":"Rub\u00e9n D\u00edez","family":"Fern\u00e1ndez","sequence":"first","affiliation":[{"name":"Departamento de Geolog\u00eda y Subsuelo Instituto Geol\u00f3gico y Minero de Espa\u00f1a (CSIC) Salamanca Spain"}]},{"given":"Carlos","family":"Fern\u00e1ndez","sequence":"additional","affiliation":[{"name":"Departamento de Geodin\u00e1mica, Estratigraf\u00eda y Paleontolog\u00eda Universidad Complutense Madrid Spain"}]},{"given":"Ricardo","family":"Arenas","sequence":"additional","affiliation":[{"name":"Departamento de Mineralog\u00eda y Petrolog\u00eda e Instituto de Geociencias (UCM, CSIC) Universidad Complutense Madrid Spain"}]},{"given":"Irene","family":"Novo\u2010Fern\u00e1ndez","sequence":"additional","affiliation":[{"name":"Departamento de Mineralog\u00eda y Petrolog\u00eda e Instituto de Geociencias (UCM, CSIC) Universidad Complutense Madrid Spain"}]}],"member":"13","published-online":{"date-parts":[[2022,1,20]]},"reference":[{"key":"e_1_2_1_7_2_1","first-page":"617","article-title":"Evoluci\u00f3n tectono\u2010metam\u00f3rfica del Corredor Blastomilon\u00edtico de Badajoz\u2010C\u00f3rdoba. 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