@article{10272/8625,
year = {2006},
url = {http://hdl.handle.net/10272/8625},
abstract = {The Pleistocene sediments deposited on the emerged marine abrasion platform near Canero village (Valdés,
Asturias) are truncated by reverse faults which are parallel to basement bedding. These structures imply a
neotectonic activity with a NW-SE maximum compressive stress, consistent with recent fault population
analysis and current seismicity studies. The described deformation corresponds to a reactivation of folds in
the Palaeozoic basement through a flexural slip mechanism, with the subsequent accommodation of the
unconformable Pleistocene cover},
publisher = {Sociedad Geológica de España},
title = {Procesos neotectónicos en los depósitos de rasa de la zona de Canero (Occidente de Asturias)},
title = {Neotectonic processes in marine terrace sediments near Canero (Western Asturias)},
author = {Gutiérrez Claverol, M. and López Fernández, Carlos and Alonso, J. L.},
}