Leioa, España
The Bartonian Ezkaba Sandstone, in the Pamplona Basin, seems to represent channel-fiIl deposits of a laterally migrating channel-Ievee turbidite system. Its siliciclastic nature and its northern derivation indicate the contemporaneous emergence of theorogenic inner-zones in the western Pyrenees.
© 2001-2024 Fundación Dialnet · Todos los derechos reservados