RT Journal Article
T1 Evolución sedimentaria reciente de las Tablas de Daimiel (Ciudad Real)
T1 Recent sedimentary evolution ofthe Tablas de Daimiel (Ciudad Real)
A1 García Hidalgo, J. F.
A1 Temiño Vela, Javier
A1 Bustamante, I. de
A1 Segura, M.
AB Two sedim entary events have been distinguished in the recent evolu tio n o f the present Tablas de Daimiel National Park. The older one is characterized by the presence of siliceous sands and silts, and mudstones; the former contain fluviatile Pelecypods and Gastropods, being interpreted as channellized deposits corresponding to the last stage of the Holocene fluvial inclssion. The mudstones sometimes contain a high content in carbonate and/or organic matter, root debris and gastropods are also common; this sediments are interpretad as deposited in a muddy alluvial plain. Finally, the younger event is dominated by peat and lime mud sedimentation in a lacustrine-palustrlne system crossed by some fluvial channels
PB Sociedad Geológica de España
YR 1995
FD 1995
LK http://hdl.handle.net/10272/13516
UL http://hdl.handle.net/10272/13516
LA spa
DS Repositorio Institucional de la Universidad de Huelva
RD 14 jul 2026