@article{10272/8988,
year = {2003},
url = {http://hdl.handle.net/10272/8988},
abstract = {Geological mapping and fades analysis of the Jurassic-Lower Cretaceous units located around the La Cantalera fossil site (Josa locality, Teruel Province, NE Spain), has allowed a precise reconstruction of a continental sedimentary basin developed around the Hauterivian-Barremian turnover. The first stage of evolution of the basin was controlled by intense normal fault activity and resulted in the formation of an isolated basin, surrounded by limestone-marly relief. The existence of a non-permanent water marshy area, with an important vegetated area, explain the abundance and diversity of the fossil remains in the studied locality},
publisher = {Sociedad Geológica de España},
keywords = {Iberian Chain},
keywords = {Synsedimentary tectonics},
keywords = {Alluvial fans},
keywords = {Vertebrates},
title = {Evolución tectosedimentaria de la Fm. Blesa (Cretàcico Inferior) en el entorno del yacimiento de vertebrados de La Cantalera (Josa, Teruel)},
title = {Tectosedìmentary evolution of the Blesa Fm. (Lower Cretaceous) around the La Cantalera fossil site (Josa, Teruel)},
author = {Bádenas, Beatriz and Canudo, José Ignacio and Ruiz Omeñaca, José Ignacio},
}