RT Journal Article
T1 Influencia diapírica sobre depósitos fluviales de tipo «braided» en la cantera de Laño (Campaniense Superior-Maastrichtiense Inferior. Cuenca Vasco-Cantábrica)
T1 Diapiric influence upon braided-type fluvial deposits at the Laño quarry (Upper Campanian-Lower Maastrichtian. Basque-Cantabrian Basin)
A1 Gómez Alday, Juan José
A1 Elorza, Javier
AB The western cliff of the Laño quarry shows extensive tabular sandsheet bodies of upper Campanian-lower Maastrichtian age, that represent channel-fill sequences deposited in a broad low-sinuosity braided-type fluvial system. Diverse sedimentological features such as channel incision, bedform types and palaeocurrent distribution, as well as the occurrence of seism related structures are interpreted in terms of possible synsedimentary tectonic activity of the very close Peñacerrada Diapir
PB Sociedad Geológica de España
YR 1998
FD 1998
LK http://hdl.handle.net/10272/10178
UL http://hdl.handle.net/10272/10178
LA spa
DS Repositorio Institucional de la Universidad de Huelva
RD 30 may 2026