@article{10272/10293,
year = {1997},
url = {http://hdl.handle.net/10272/10293},
abstract = {A detailed mapping of the Zufia Formation near Estella-Lizarra (Navarra) has led to the discovery of a shallow-water marine carbonate-terrigenous unit of early Cenomanian age. The Aramendia unit consists basically of calcarenites. Facies analysis, lateral and vertical distribution are used to build a sedimentary model of a carbonate shoal. The calcarenitic shoal separates two principal domains: 7/ to the south, a back-shoal trough with calcarenitic material exported from the shoal and terrigenous input derived from the terrestrial hinterland, and 2/ a deeper fore-shoal trough with marly sedimentation and occasional intercalation of shoal derived beds. This fore-shoal area is devoid of terrigenous input after the shoal-barrier effect. A tectonic control influenced the foundation of the shoal on a structural paleohigh},
publisher = {Sociedad Geológica de España},
keywords = {Carbonate shoal},
keywords = {Sedimentary model},
keywords = {Tectonic control},
keywords = {Lower Cenomanian},
keywords = {Estella-Lizarra},
keywords = {Spain},
title = {El modelo de bajío calcarenítico de Aramendia (Cenomaniense inferior, Estella-Lizarra, Navarra)},
title = {The Aramendia calcarenite-shoal model (early Cenomanian, Estella-Lizarra, Navarra)},
author = {López Horgue, Mikel A. and Fernández Mendiola, Pedro Ángel and García Mondéjar, Joaquín},
}