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- W2187537265 abstract "Extensive alluvial outcrops of the Lower Guadalquivir River constitute a complex system of terraces, placed in the left margin of the river. The current floodplain is placed in outlying position. The highest and most distant from the current riverbed terraces are placed about 140 meters above the floodplain and have been attributed to the Late Pleistocene. This position can be explained by upward and tilting towards NW and N of the terrace system, which would have provoked the migration of the Guadalquivir River during Quaternary times. The evolution of the Low Guadalquivir fluvial system can be related to the recent tectonic evolution of western Betics, since the river course and the plan distribution of different terraces follow the structural trend of Gibraltar Arch and the migration of the Betic deformation front." @default.
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- W2187537265 date "2013-01-01" @default.
- W2187537265 modified "2023-09-27" @default.
- W2187537265 title "Análisis geomorfológico de las terrazas fluviales del Bajo Guadalquivir e implicaciones tectónicas Geomorphologic analysis of the fluvial terraces of the Lower Guadalquivir River and tectonics implications" @default.
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