@article{10272/8689,
year = {2005},
url = {http://hdl.handle.net/10272/8689},
abstract = {La Zubia alluvial fan is located at the boundary between the western slopes of Sierra Nevada and the
Granada depression. The Alpujárride rocks of the northwestern flank of Sierra Nevada antiform constitute
its metamorphic basement. New gravity data allow to estimate the distribution of the Neogene-Quaternary
sedimentary fill thickness. Gravity models indicate that the N-S normal faults of Sierra Nevada border have
not large related depocenters and the basement is deeper towards the Granada depression. Faults are
more active in the northern sector of the alluvial fan, where is located the NW-SE oriented Granada Fault
that northwestwards progressively increases its vertical slip.},
publisher = {Sociedad Geológica de España},
title = {Anomalías gravimétricas y estructura del abanico aluvial de La Zubia (Sierra Nevada occidental, Cordilleras Béticas)},
title = {Gravity anomalies and structure of the La Zubia alluvial fan (western Sierra Nevada, Betic Cordilleras)},
author = {Ruiz Constán, Ana and Galindo Zaldívar, Jesús and Sanz de Galdeano, Carlos},
}