RT Journal Article
T1 Las tobas cuaternarias del río Añamaza (provincia de Soria, Cordillera Ibérica): aproximación cronológica
T1 Quaternary tufas of the River Añamaza (NW Iberian Ranges, Spain): a chronological approach
A1 Arenas Abad, Concepción
A1 Sancho, Carlos
A1 Vázquez Urbez, Marta
A1 Pardo, Gonzalo
A1 Hellstrom, John
A1 Ortiz, José Eugenio
A1 Torres, Trinidad de
A1 Osácar, María Cinta
A1 Auqué Sánz, Luis
AB High-gradient, stepped fluvial tufa systems with dammed areas existed in the River Añamaza valley(NW Iberian Ranges, Spain) during Quaternary times. Single deposits range from a few meters to about 70m thick, in which prograding-aggrading wedges separated by erosional surfaces exist. Several episodes oftufa formation have been distinguished by means of U-series, Amino-acid racemization and radiocarbontechniques. These correlate to MIS 8, 7, 5 and 1. The presence of MIS 9 is uncertain, as chronological datamay also correspond to older stages. Most tufas in this area formed in MIS 5. Distinct tufa episodes canalso be distinguished in the Holocene. These are the first chronological data presented for one of thenorthernmost Quaternary tufa systems in the Iberian Ranges
PB Universidad de Huelva
YR 2010
FD 2010
LK http://hdl.handle.net/10272/7477
UL http://hdl.handle.net/10272/7477
LA spa
DS Repositorio Institucional de la Universidad de Huelva
RD 30 may 2026