@article{10272/11092,
year = {1996},
url = {http://hdl.handle.net/10272/11092},
abstract = {The turbidite equivalent of the Figols Allogroup can be recognized at the base ofthe Hecho Croup. Three deposition a! sequences -Figols 1,2 and 3- are recorded and are organized in third order stages of growth. All the sequences have similar features in the first stage. Lower boundaries are tectonically induced. A sudden zonal basinward shifting occurs and depositional systems (lobes) are developed. Second and third stages are well developed in Figols 2 and 3. The second stages record a strong and progressive landward shifting in both systems and the third stages are the basinat expression of the foreland carbonate ramps},
publisher = {Sociedad Geológica de España},
title = {Presencia del Alogrupo de Figols en las turbiditas de la base del Grupo de Hecho (Barranco del Sorrosal, Prov. de Huesca)},
title = {Occurrence ofthe Figols Allogroup in the basa! turbidites ofthe Hecho Group (Barranco del Sorrosal, Huesca Prov.)},
author = {Remacha Grau, Eduard and Raïmat, C. and Oms, O. and Cardona, D. and Mutti, E.},
}