scispace - formally typeset
A

Aurora Rodrigues

Researcher at University of São Paulo

Publications -  39
Citations -  1276

Aurora Rodrigues is an academic researcher from University of São Paulo. The author has contributed to research in topics: Sediment & Continental shelf. The author has an hindex of 15, co-authored 35 publications receiving 1175 citations.

Papers
More filters
Journal ArticleDOI

Coast line evolution in Portugal since the Last Glacial Maximum until present — a synthesis

TL;DR: In this paper, an effort has been made to assemble a data set on the evolution of coastal morphology of the West Iberian Continental Margin in Portugal, which has occurred since the Last Glacial Maximum.
Journal ArticleDOI

Clay minerals from the sedimentary cover from the Northwest Iberian shelf

TL;DR: In this article, the distributions of clay mineral in the top layer of the sedimentary cover are shown to be related to their continental sources, but also reflect the influences of winter storms and longshore currents in determining the pathways of sediment transport.
Journal ArticleDOI

Present day sedimentary processes on the northern Iberian shelf

TL;DR: In this article, the authors describe the mechanisms controlling the deposition of the fine-grained sediment depositions and the processes that result in resuspension processes on the Galicia-Minho Shelf.
Journal ArticleDOI

Dispersal and deposition of suspended sediment on the shelf off the Tagus and Sado estuaries, S.W. Portugal

TL;DR: In this article, the authors estimate the amount of suspended particulate matter being discharged annually from the Tagus estuary to be between 0.4 and 1×10 6 t.
Journal ArticleDOI

Sedimentary particle distribution and dynamics on the Nazaré canyon system and adjacent shelf (Portugal)

TL;DR: In this paper, a conceptual model was proposed to delineate the mechanisms acting in this particular area, taking into account three different sources of material to the Nazare canyon: 1. upwelling conditions, resuspension of middle shelf deposits by internal wave activity and transport to the canyon in the BNL; 2.erosion of northern/southern beach and sea cliff materials transported by littoral drift to the Canyon head and 3. fine sediment input from the southern river and transport during downwelling condition (winter).