Wide-angle seismic studies have determined the detailed velocity structure along a 350-km-long profile across the Labrador margin. Combination of this model...
The crust across each margin of the Labrador Sea, a conjugate rift margin pair, consists of three well-defined zones: thinned continental crust, 70-80-km-wide...
The crustal velocity structure beneath western Newfoundland is constrained by a reanalysis of older, regional refraction profiles together with an analysis of...
We calculate the anomalous basement topography for the North Atlantic Ocean from 30° to 70°N latitude and from 0° to 70°W longitude at a resolution of roughly...
The Nova Scotia continental margin off eastern Canada marks a transition from a volcanic to a nonvolcanic style of rifting. The northern (nonvolcanic) segment...
Two seismic refraction lines were acquired along and across the extinct Labrador Sea spreading center during the Seismic Investigations off Greenland,...
The central Nova Scotia margin off Eastern Canada is located at a transition from a volcanic margin in the south to a non-volcanic margin in the north. In...
We present a joint analysis of seismic reflection and refraction profiles across an extinct spreading center in the Labrador Sea. The refraction data are used...
In 2009, the SIGNAL (Seismic Investigations off Greenland, Newfoundland and Labrador) experiment was carried out to acquire marine refraction seismic data in...
Actes de conférence
Texte intégral en ligne
Filtrer vos résultats
Opération réussie
L’élément a été sauvegardé.
Opération réussie
Cet élément a été retiré.
Erreur
Vous avez dépassé le nombre maximal de 100 résultats sauvegardés.
Erreur
Impossible de sauvegarder l’élément. Veuillez réessayer. Si le problème persiste, il pourrait y avoir un problème avec l’élément.
Erreur
Impossible de supprimer l’article demandé. Veuillez réessayer plus tard.