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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Cited articles

Alcock, J. E., Martínez Catalán, J. R., Arenas, R., and Díez Montes, A.: Use of thermal modeling to assess the tectono-metamorphic history of the Lugo and Sanabria gneiss domes, Northwest Iberia, Bull. Soc. Geol. Fr., 180, 179–197, https://doi.org/10.2113/gssgfbull.180.3.179, 2009. 
Alcock, J. E., Martínez Catalán, J. R., and Arenas, R.: One- and two-dimensional models are equally effective in monitoring the crust's thermal response to advection by large-scale thrusting during orogenesis, Comput. Geosci., 37, 1205–1207, https://doi.org/10.1016/j.cageo.2011.02.012, 2011. 
Alcock, J. E., Martínez Catalán, J. R., Rubio Pascual, F. J., Díez Montes, A., Díez Fernández, R., Gómez Barreiro, J., Arenas, R., Dias da Silva, Í., and González Clavijo, E.: 2-D thermal modeling of HT-LP metamorphism in NW and Central Iberia: Implications for Variscan magmatism, rheology of the lithosphere and orogenic evolution, Tectonophysics, 657, 21–37, https://doi.org/10.1016/j.tecto.2015.05.022, 2015. 
Alonso, J. L.: Sequences of thrusts and displacement transfer in the superposed duplexes of the Esla Nappe Region (cantabrian zone, nw spain), J. Struct. Geol., 9, 969–983, https://doi.org/10.1016/0191-8141(87)90005-8, 1987. 
Alonso, J. L., Marcos, A., and Suárez, A.: Paleogeographic inversion resulting from large out of sequence breaching thrusts: The León Fault (Cantabrian zone, NW Iberia). A new picture of the external Variscan thrust belt in the Ibero-Armorican arc, Geol. Acta, 7, 451–473, https://doi.org/10.1344/105.000001449, 2009. 
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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.
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