RT Journal Article
T1 Procedencia de los materiales terrígenos finos del Paleógeno continental, zona de Vic, NE España
T1 Provenance of non-marine Palaeogene fine-grained clastic materials, Vic area, NE Spain
A1 Balañá, J.
A1 Colombo Piñol, Ferrán
A1 Vaquer, R.
AB In the Vic area, the non-marine Palaeogene clastic materials are arranged in two successive lithostratigraphicformations: the lower, Vilanova de Sau (VS) mainly composed of lutites and some channels of sandstones,and the upper, Romagats (RO) mainly consisting of conglomeratic sandstones with few lutitic intercalations.The VS is interpreted as distal and lateral alluvial fan facies, whereas the RO is regarded as alluvial fanproximal facies. The clay mineral analysis, the study of the main palaeocurrents and the different clastlithologies distribution along the studied stratigraphic logs suggest that the source area was located to theeast of the present outcrops. In addition, the geochemical analysis of the fine-grained materials providemore evidence that the main source area was placed eastwards, at the area at present occupied by theMediterranean sea and relatively near the coast
YR 2006
FD 2006
LK http://hdl.handle.net/10272/8516
UL http://hdl.handle.net/10272/8516
LA spa
DS Repositorio Institucional de la Universidad de Huelva
RD 30 may 2026