RT Journal Article
T1 Anomalías gravimétricas y estructura del abanico aluvial de La Zubia (Sierra Nevada occidental, Cordilleras Béticas)
T1 Gravity anomalies and structure of the La Zubia alluvial fan (western Sierra Nevada, Betic Cordilleras)
A1 Ruiz Constán, Ana
A1 Galindo Zaldívar, Jesús
A1 Sanz de Galdeano, Carlos
AB La Zubia alluvial fan is located at the boundary between the western slopes of Sierra Nevada and theGranada depression. The Alpujárride rocks of the northwestern flank of Sierra Nevada antiform constituteits metamorphic basement. New gravity data allow to estimate the distribution of the Neogene-Quaternarysedimentary fill thickness. Gravity models indicate that the N-S normal faults of Sierra Nevada border havenot large related depocenters and the basement is deeper towards the Granada depression. Faults aremore active in the northern sector of the alluvial fan, where is located the NW-SE oriented Granada Faultthat northwestwards progressively increases its vertical slip.
PB Sociedad Geológica de España
YR 2005
FD 2005
LK http://hdl.handle.net/10272/8689
UL http://hdl.handle.net/10272/8689
LA spa
DS Repositorio Institucional de la Universidad de Huelva
RD 31 may 2026