Articles | Volume 12, issue 7
https://doi.org/10.5194/se-12-1515-2021
https://doi.org/10.5194/se-12-1515-2021
Research article
 | 
06 Jul 2021
Research article |  | 06 Jul 2021

Evolution of the Iberian Massif as deduced from its crustal thickness and geometry of a mid-crustal (Conrad) discontinuity

Puy Ayarza, José Ramón Martínez Catalán, Ana Martínez García, Juan Alcalde, Juvenal Andrés, José Fernando Simancas, Immaculada Palomeras, David Martí, Irene DeFelipe, Chris Juhlin, and Ramón Carbonell

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AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by Puy Ayarza on behalf of the Authors (05 Mar 2021)  Author's response   Author's tracked changes   Manuscript 
ED: Referee Nomination & Report Request started (07 Mar 2021) by Irene Bianchi
RR by Anonymous Referee #1 (04 May 2021)
ED: Publish subject to minor revisions (review by editor) (05 May 2021) by Irene Bianchi
AR by Puy Ayarza on behalf of the Authors (17 May 2021)  Author's response   Author's tracked changes   Manuscript 
ED: Publish as is (19 May 2021) by Irene Bianchi
ED: Publish as is (27 May 2021) by Federico Rossetti (Executive editor)
AR by Puy Ayarza on behalf of the Authors (28 May 2021)  Manuscript 
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Short summary
Vertical incidence seismic profiling on the Iberian Massif images a mid-crustal-scale discontinuity at the top of the reflective lower crust. This feature shows that upper- and lower-crustal reflections merge into it, suggesting that it has often behaved as a detachment. The orogen-scale extension of this discontinuity, present in Gondwanan and Avalonian affinity terranes into the Iberian Massif, demonstrates its relevance, leading us to interpret it as the Conrad discontinuity.