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This structure formed after primary (protolith) and secondary (tectonometamorphic) processes during the extensional collapse of the Variscan Orogen. The SPCS structure is usually controlled by foreland\u2010directed thrusts and strike\u2010slip faults. However, the eastern SPCS is dominated by NW\u2010directed, imbricate backthrusts and lacks the main thrust directed to the foreland basin located southeast of the mountain range (Madrid Cenozoic Basin). The SPCS exhibits a crustal root (&gt;40\u00a0km depth) supporting SE\u2010directed crustal\u2010scale thrusting. Alpine backthrusts sole into an SE\u2010dipping d\u00e9collement within the Variscan basement. Variscan extension\u2010related structures parallel the SE\u2010dipping geometry of Alpine backthrusts, so they provided favorably oriented rheological weaknesses to accommodate Alpine shortening. Backthrusts geometry, their hanging wall position within the fault that raised the SPCS and gravity modeling support an Alpine crustal delamination process. Tectonic wedging and delamination of the more competent basement occurred in the footwall of Variscan extensional faults (Daurius domain), which enforced the shearing off of a rheologically weaker upper layer of the crust, located in the hanging wall of the Variscan extensional faults (Arriaca domain) by inverting Variscan extensional faults. This led to NW\u2010directed incipient continental subduction of the weaker crust. Intraplate subduction and crustal delamination can be independent from lithosphere\u2010scale inheritance and be conditioned by structural inheritance in the overlying crust. Alpine shortening for the Cretaceous cover is around 17.7\u00a0km (10.5% shortening), and 11\u00a0km (7%) for the upper\u2010lower crust limit.<\/jats:p>","DOI":"10.1029\/2022tc007315","type":"journal-article","created":{"date-parts":[[2022,7,20]],"date-time":"2022-07-20T08:01:31Z","timestamp":1658304091000},"update-policy":"https:\/\/doi.org\/10.1002\/crossmark_policy","source":"Crossref","is-referenced-by-count":4,"title":["Variscan Inheritance Induces Alpine Upper Crustal Delamination in East Spanish\u2010Portuguese Central System"],"prefix":"10.1029","volume":"41","author":[{"ORCID":"https:\/\/orcid.org\/0000-0002-7198-8517","authenticated-orcid":false,"given":"G.","family":"de Vicente","sequence":"first","affiliation":[{"name":"GEODESPAL Facultad de C.C. Geol\u00f3gicas Universidad Complutense de Madrid Madrid Spain"},{"name":"Instituto de Geociencias IGEO. CSIC\u2010UCM Madrid Spain"}]},{"ORCID":"https:\/\/orcid.org\/0000-0002-0379-7970","authenticated-orcid":false,"given":"R. 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