Aportació al coneixement de l'evolució geològica recent de la plana del Ter (Baix Empordà)

The infilling of the river Ter Plain was produced by alluvial systems under the control of sea-level changes during the Quaternary. This paper describes the sedimentary evolution of the plain, and attemps to present a chronology of the recent geological events based on eustatic curves ​
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