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...
Autor principal: | |
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Outros Autores: | , , , , , , , |
Formato: | article |
Idioma: | eng |
Publicado em: |
2022
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Assuntos: | |
Texto completo: | http://hdl.handle.net/10451/51471 |
País: | Portugal |
Oai: | oai:repositorio.ul.pt:10451/51471 |