FN Archimer Export Format
PT J
TI The French Atlantic margin and deep-sea submarine systems
BT 
AF BOURILLET, Jean-Francois
   ZARAGOSI, S
   MULDER, T
AS 1:1;2:2;3:2;
FF 1:PDG-DOP-DCB-GM-LES;2:;3:;
C1 IFREMER, Lab Evironm Sedimentaires, F-29280 Plouzane, France.
   Univ Bordeaux 1, Dept Geol & Oceanog, UMR 5805, EPOC, F-33405 Talence, France.
C2 IFREMER, FRANCE
   UNIV BORDEAUX, FRANCE
SI BREST
SE PDG-DOP-DCB-GM-LES
IN WOS Ifremer jusqu'en 2018
   copubli-france
   copubli-univ-france
IF 0.677
TC 38
TU Centre national de la recherche scientifique
   Université de Bordeaux
   École pratique des hautes études
UR https://archimer.ifremer.fr/doc/2006/publication-2137.pdf
LA English
DT Article
CR MD 133 / SEDICAR
   MD 141 / ALIENOR 1
BO Marion Dufresne
DE ;Sedimentology;Geomorphologya;Deep sea;Bay of Biscay;French Atlantic margin
AB The sedimentary infill of the Bay of Biscay off Ireland, UK, France and Spain took place in four phases. The last one (35 Ma to present) is characterised by gravitational, pelagic, contouritic and glacigenic processes leading to the setup of three deep sea systems. To the North, the Celtic and Armorican fans are fed by a "canyon-dominated" margin and its connection with the "Manche" palaeoriver, which drained a large area of western Europe. To the South, the Cap-Ferret fan results from the evolution of a "tectonic-dominated" margin and the erosion of the Pyrenee mountains.
PY 2006
PD DEC
SO Geo-Marine Letters
SN 0276-0460
PU Springer
VL 26
IS 6
UT 000242295400002
BP 311
EP 315
DI 10.1007/s00367-006-0042-2
ID 2137
ER

EF