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dedup_wf_001--e6cbf150783aad6e211ec498bd44ac14
The NW Iberian margin is a hyperextended continental margin, formed during the opening of the North Atlantic Ocean, where a subsequent partial tectonic inversion has undergone... -
Bouguer anomalies of the NW Iberian continental margin and the adjacent abyss...
The NW Iberian continental margin has a complex structure, resulting from the succession of several rifting episodes close to a ridge triple junction, and a superimposed partial...