@article{10272/14015,
year = {1994},
url = {http://hdl.handle.net/10272/14015},
abstract = {The "Nivel de Fuentes", in the Valdelacasa Allogroup (Precambrian-Cambrian), can be divided in five subunits. Each one of them is build-up by a basal megabreccia overlaid by a fine-grained turbidite wedge that tends to pinch-out toward the central region of the Valdelacasa anticline. The isochron character ofthe "Nivel de Fuentes" is rejected because really it is multievent},
publisher = {Sociedad Geológica de España},
title = {Variaciones laterales del "Nivel de Fuentes", Precámbrico-Cámbrico de la Zona Centro-Ibérica},
title = {Lateral changes in the "Nivel de Fuentes", Precambrían-Cambrían ofthe Central-Iberian Zone.},
author = {Santamaría Casanovas, J. and Remacha Grau, Eduard},
}