RT Journal Article
T1 Carbonatos palustres en llanuras de inundación fluviales del Plioceno-Pleistoceno (Cuenca de Guadix, Granada, España)
T1 Palustrine carbonates within Pliocene-Pleistocene fluvial floodplains(Guadix Basin, Granada, Spain)
A1 Pla Pueyo, Sila
A1 Yébenes, Alfonso
A1 Soria, Jesús M.
A1 Viseras, César
AB During its continental stage of infilling (Late Tortonian-Late Pleistocene), the Guadix Basin acted as anendorheic depression in which an axial fluvial system, fed partialy by two transverse alluvial systems,drained towards a large shallow lake located in the eastern sector. At that moment, detritic and carbonatesediments were depositing in the floodplains of the axial valley. The study of the carbonate facies showsthat most of them were deposited in palustrine environments. The palustrine carbonate sediments havebeen characterized according to their degree of pedological modification and to their content in detriticcomponents. Some of the palustrine sediments appear to be related to the progradation of the transversealluvial fans, which eventually gave way to the blocking of the master drainage towards the east andthe temporary development of extensive ponds
YR 2007
FD 2007
LK http://hdl.handle.net/10272/8340
UL http://hdl.handle.net/10272/8340
LA spa
DS Repositorio Institucional de la Universidad de Huelva
RD 30 may 2026