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...
Main Author: | |
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Other Authors: | , , , , , , , |
Format: | article |
Language: | eng |
Published: |
2022
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Subjects: | |
Online Access: | http://hdl.handle.net/10451/51471 |
Country: | Portugal |
Oai: | oai:repositorio.ul.pt:10451/51471 |