@article{10272/7460,
year = {2010},
url = {http://hdl.handle.net/10272/7460},
abstract = {A conglomeratic level intercalated in a turbiditic sequence in the Almanzora corridor (Betic Cordillera)
has been mapped. This level is 3 to 15 m thick, with clasts bigger than 3 m diameter. It can be continued
along 6 km, which makes it being a good key bed in the study area. The level origin has been interpreted
as a collapse deposit from the southern margin of the basin, probably due to a seismic event},
publisher = {Universidad de Huelva},
title = {Caracterización sedimentológica de un nivel guía y su posible origen sísmico, Corredor del Almanzora (Almería)},
title = {Sedimentologic characterization of a key bed: a possible seismic origin (Almanzora Corridor, Almería)},
author = {Sola, Fernando},
}