@article{10272/10288,
year = {1997},
url = {http://hdl.handle.net/10272/10288},
abstract = {The Aptian of Lanestosa is analyzed based on detailed mapping and facies analysis. Four sedimentary units are differentiated: a basal terrigenous unit and three overlying carbonate platform units. Units boundaries 2-3 and 3-4 represent unconformity surfaces linked to synsedimentary tectonic activity. The Cabuerniga-Ramales E-W trending fault is responsible of the repeated block tilting in mid Aptian and late Aptian times. The origin of Pb-Zn ores in this area is likely related to this tectonic activity},
publisher = {Sociedad Geológica de España},
title = {El Aptiense de Lanestosa (Bizkaia): implicaciones paleotectónicas},
title = {The Aptian of Lanestosa (Bizkaia): palaeotectonic implications},
author = {López Horgue, Mikel A. and Fernández Mendiola, Pedro Ángel and García Mondéjar, Joaquín},
}