A tectonic carpet of Variscan flysch at the base of a rootless accretionary prism in northwestern Iberia: U–Pb zircon age constrains from sediments and volcanic olistoliths

The allochthonous complexes of Galicia–Trás-os-Montes Zone (NW Iberia) are part of a rootless tectonic stack which preserves part of a Variscan accretionary prism. They are formed by individual tectonic slices marked by specific tectonometamorphic evolutions, which were piled up in a piggy-back mode...

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Detalhes bibliográficos
Autor principal: Clavijo, Emilio (author)
Outros Autores: Silva, Ícaro (author), Martínez Catalán, José R. (author), Gómez Barreiro, Juan (author), Gutiérrez-Alonso, Gabriel (author), Díez Montes, Alejandro (author), Hofmann, Mandy (author), Gärtner, Andreas (author), Linnemann, Ulf (author)
Formato: article
Idioma:eng
Publicado em: 2022
Assuntos:
Texto completo:http://hdl.handle.net/10451/51471
País:Portugal
Oai:oai:repositorio.ul.pt:10451/51471