FN Archimer Export Format
PT J
TI Quaternary turbidite systems on the northern margins of the Balearic Basin (Western Mediterranean): a synthesis
BT 
AF DROZ, Laurence
   DOS REIS, A. T.
   RABINEAU, Marina
   BERNE, Serge
   BELLAICHE, G
AS 1:1;2:2;3:1;4:3;5:4;
FF 1:;2:;3:;4:PDG-DOP-DCB-GM-LES;5:;
C1 Inst Univ Europeen Mer, CNRS, UMR 6538, F-29280 Plouzane, France.
   Universidade do Estado do Rio de Janeiro Brazil, Dept Oceanog, BR-22550900 Rio De Janeiro, Brazil.
   IFREMER, Lab Environm Sedimentaires, F-29280 Plouzane, France.
   CNRS, UMR 6526, GEOSCI AZUR, F-06235 Villefranche Sur Mer, France.
C2 IUEM, FRANCE
   UNIV RIO DE JANEIRO, BRAZIL
   IFREMER, FRANCE
   CNRS, FRANCE
SI BREST
SE PDG-DOP-DCB-GM-LES
IN WOS Ifremer jusqu'en 2018
   copubli-france
   copubli-univ-france
   copubli-int-hors-europe
   copubli-sud
IF 0.677
TC 29
TU CNRS
   IFREMER
   IRD
   IUEM
   OBSERVATOIRE DE LA COTE D'AZUR
   SCEF HYDROGRAPH OCEANOGRAPHIQUE MARINE
   UNIVERSITE AIX-MARSEILLE
   UNIVERSITE BREST
   UNIVERSITE BRETAGNE-SUD
   UNIVERSITE NICE
   UNIVERSITE PARIS 6
UR https://archimer.ifremer.fr/doc/2006/publication-2171.pdf
LA English
DT Article
CR PROGRES
   PROMESS 1
BO Le Suroît
   Bavenit
DE ;Gulf of Lion;Quaternary evolution;Turbidity;Sedimentary system
AB The Balearic Basin is a young basin composed of thick Plio-Quaternary sediments, including active gravity sedimentation. During the Quaternary, gravity processes deposited (1) turbidite systems, either as symmetrical fans (Petit-Rhone and Valencia fans) or asymmetrical ridges (Marseille-Planier, Grand- Rhone and Pyreneo-Languedocian ridges) and (2) several mass-transport deposits, indicating recurrent sedimentary failures of the margin. This paper synthesizes previous works and proposes a chronological sedimentary evolution for the basin. Except for the last 20 ka, the chronostratigraphy remains poorly constrained but should soon be established for the last 500 ka, based on the PROMESS1 drillings on the outer shelf of the Gulf of Lions, and hopefully for the last 30 Ma, based on ultra-deep drilling in the deep basin from aboard the Chikyu research vessel (IODP proposal Pre699).
PY 2006
PD DEC
SO Geo-Marine Letters
SN 0276-0460
PU Springer
VL 26
IS 6
UT 000242295400005
BP 347
EP 359
DI 10.1007/s00367-006-0044-0
ID 2171
ER

EF