Data/hora: 11/06/2024 02:30:19

Provedor de dados: 	5	
País: 	France	
Título: 	La marge du Grand Banc et la fracture de Terre-Neuve	
Autores: 	Auzende, Jean-marie; Olivet, Jean-louis; Bonnin, Jean.	
Data: 	1970-09	
Ano: 	1970	
Palavras-chave: 	Histoire Ifremer.	
Resumo: 	Some seismic and magnetic profiles carried out south of the Big Bank of Newfoundland during the Noratlante cruise show a fracture zone which collapses the continental margin and continues to the south-east towards the Azores. This fracture zone proves evidence of the drift movement of Africa towards the east during the Jurassic or Trias opening of the Atlantic. From the south-east corner of the Big Bank, the fracture zone supports a sediment ridge formed by the underflows and which continues to the meridian 430 West.	
Tipo: 	Text	
Idioma: 	Francês	
Identificador: 	http://archimer.ifremer.fr/doc/1970/publication-4877.pdf	
Editor: 	Académie des Sciences	
Relação: 	http://archimer.ifremer.fr/doc/00000/4877/	
Formato: 	application/pdf	
Fonte: 	Comptes Rendus Académie des Sciences de Paris (Académie des Sciences), 1970-09 , Vol. 271 , P. 1063-1066	
Fonte: 	Académie des Sciences