RT Journal Article
T1 Las Facies fluviales de las unidades Superior Terciariay Pliocuaternaria de la Cuenca del Guadiana entre Mériday Badajoz (España)
A1 Moya Palomares, María Eugenia
A1 Azevêdo, M.T.
A1 Rodríguez Plaza, María Jesús
AB This paper describe two units of the Guadiana Basin (Cenozoic) between Mérida and Badajoz, Spain. The first unit (upper tertiary unit) represent fluvial sandstone deposits that was migrating from the E towards the W. The miocene fluvial system is characterised for channels and bars deposits associated with edafic levels and erratic development of the flood plain deposits. The second fluvial unit (plioquaternary unit) represent a new superimposed fluvial system. The Plioquaternary system is characterised for sandstone and conglomeratic deposits that represent channel and bars with high lateral displacements as consequence of the migration and fill of the fluvial system. Both types of fluvial systems represent part of the evolution of the Guadiana basin from the Miocene until the Plioquaternary.
PB Sociedad Geológica de España.
SN 1576-5172
YR 2000
FD 2000
LK https://hdl.handle.net/20.500.14352/58000
UL https://hdl.handle.net/20.500.14352/58000
LA spa
DS Docta Complutense
RD 29 abr 2024