RT Journal Article
T1 Secuencia de cabalgamientos en la Zona Sub-Atlásica y cuenca de Ouarzazate; borde sur del Alto Atlas (Marruecos)
A1 Tesón, E.
A1 Teixell, Antonio
AB The Sub-Atlas thrust belt and Ouarzazate basin constitutes the best and almost the unique synorogenicrecord of the Atlas mountain building. During the Eocene and Oligocene the deformation was concentredin the distant High Atlas whereas the marginal thrust belt was scarcely deformed. In Late Oligocene toearly Miocene, deformation migrated forelandwards when complex thrust sequences created the Sub-Atlas foreland fold and thrust belt. Thrusting took place up to Pliocene times entraining the synorogenicsedimentary rocks, locally-sourced terrigenous and lacustrine deposits
PB Sociedad Geológica de España
YR 2006
FD 2006
LK http://hdl.handle.net/10272/8630
UL http://hdl.handle.net/10272/8630
LA spa
DS Repositorio Institucional de la Universidad de Huelva
RD 13 jun 2026