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- W2341644894 abstract "The geometry, structures and tectonic evolution of the western termination of the Alpine-Pyrenean Orogen relief onshore and related foreland have been studied. We present the results of structural mapping and detailed outcrop studies of Cenozoic-age structures carried out at the NW Iberian Peninsula. On the basis of this work we propose a new tectonic model for the termination. a N-S-oriented arch-shape structures (Ibias-Ancares and Rua-Vilalba). Tectonic activity commenced during the Eocene, and in the westernmost areas during the Late Oligocene. The CM south-verging thrust activity ended at the beginning of Late Miocene, al- though deformation continued in the GLM with north-verging thrusts. The evidence of intense tectonic activity during the Miocene, the western migration and southward transference of tectonic activity and the interaction of two successive deformation fronts, suggests that a re-examination of the tectonic evolution of the northern Iberian microplate during the Alpine Orogeny is necessary." @default.
- W2341644894 created "2016-06-24" @default.
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- W2341644894 date "2011-01-01" @default.
- W2341644894 modified "2023-09-27" @default.
- W2341644894 title "Geometry, structures and evolution of the western termination of the Alpine-Pyrenean Orogen reliefs (NW Iberian Peninsula) Geometría, estructuras y evolución de la terminación occidental de los relieves del Orógeno Alpino-Pirenaico (NO Península Ibérica)" @default.
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