Salt tectonics, a controlling factor on the development of the Marseilles and Grand-Rhone sedimentary ridges, Gulf of Lions, western Mediterranean Sea;Rôle de la tectonique salifère dans la construction des rides sédimentaires de Marseille et du Grand Rhône, golfe du Lion, Méditerranée occidentale

Comptes Rendus - Geoscience

Volumn 336, Issue 2, 2004, Pages 143-150

  dos Reis, Antonio Tadeu ^a   Gorini, Christian ^b   Mauffret, Alain ^c   Weibull, Wiktor ^a  

^a STATE UNIVERSITY OF RIO DE JANEIRO   (Brazil)

^b UNIV LILLE   (France)

^c SORBONNE UNIVERSITÉ   (France)

Author keywords

France; Gulf of Lions; Marseilles and Grand Rhone ridges; Salt tectonics; Salt sediment interaction

Indexed keywords

SALT TECTONICS; SEDIMENTATION; SUBMARINE RIDGE;

GULF OF LION; MEDITERRANEAN SEA;

EID: 1342310538     PISSN: 16310713     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.crte.2003.10.022     Document Type: Article

References (1)

1. Bellaiche G. Coutellier V. Droz L. Detailed morphology, sedimentary structure and evolution of the continental margin of the Western Provencal Bassin (south of France) since Late Miocene Mar. Geol. 89 1989 259-268