FN Archimer Export Format
PT J
TI Messinian evaporite deposition during sea level rise in the Gulf of Lions (Western Mediterranean)
BT 
AF BACHE, Francois
   GARGANI, Julien
   SUC, Jean-Pierre
   GORINI, Christian
   RABINEAU, Marina
   POPESCU, Speranta-Maria
   LEROUX, Estelle
   DO COUTO, Damien
   JOUANNIC, Gwenael
   RUBINO, Jean-Loup
   OLIVET, Jean-Louis
   CLAUZON, Georges
   DOS REIS, Antonio Tadeu
   ASLANIAN, Daniel
AS 1:1;2:2;3:3,4;4:3,4;5:5;6:6;7:5,7;8:3,4,8;9:2,9;10:10;11:7;12:11;13:12;14:7;
FF 1:;2:;3:;4:;5:;6:;7:;8:;9:;10:;11:;12:;13:;14:PDG-REM-GM-LGG;
C1 GNS Sci, Lower Hutt 5040, New Zealand.
   Univ Paris 11, Lab GEOPS, UMR 8148, F-91405 Orsay, France.
   Univ Paris 11, Univ Paris 04, Inst Sci Terre Paris iSTeP, UMR 7193, F-75005 Paris, France.
   CNRS, Inst Sci Terre Paris iSTeP, UMR 7193, F-75005 Paris, France.
   IUEM, Domaines Ocean UMR 6538, F-29280 Plouzane, France.
   Geobiostrat Data Consulting, F-69140 Rillieux La Pape, France.
   IFREMER, Geosci Marines, LGG, F-29280 Plouzane, France.
   TOTAL, F-92400 Paris, France.
   CETE Est, LRPC, Nancy, France.
   TOTAL, TG ISS, CSTJF, F-64018 Pau, France.
   Aix Marseille Univ, CNRS, IRD, CEREGE UM34, F-13545 Aix En Provence, France.
   Dept Oceanog Geol UERJ Brazil, BR-20550900 Rio De Janeiro, RJ, Brazil.
C2 GNS SCI, NEW ZEALAND
   UNIV PARIS 11, FRANCE
   UNIV PARIS 11, FRANCE
   CNRS, FRANCE
   UBO, FRANCE
   GEOBIOSTRATDATA CONSULTING, FRANCE
   IFREMER, FRANCE
   TOTAL, FRANCE
   CETE EST, FRANCE
   TOTAL, FRANCE
   UNIV AIX MARSEILLE, FRANCE
   UERJ BRAZIL, BRAZIL
SI BREST
SE PDG-REM-GM-LGG
UM LGO
IN WOS Ifremer jusqu'en 2018
   copubli-france
   copubli-univ-france
   copubli-int-hors-europe
   copubli-sud
IF 2.788
TC 43
UR https://archimer.ifremer.fr/doc/00248/35887/34408.pdf
LA English
DT Article
CR AM-MED-1
   MONICYA
   SARDINIA
BO Le Suroît
   Le Noroit
   L'Atalante
DE ;Messinian;Mediterranean;Gulf of Lions;Seismic stratigraphy;Evaporites
AB The Messinian Salinity Crisis resulted from desiccation of the Mediterranean Sea after its isolation from the Atlantic Ocean at the end of the Miocene. Stratal geometry tied to borehole data in the Gulf of Lions show that the pre-crisis continental shelf has been eroded during a major sea-level fall and that sediments from this erosion have been deposited in the basin. This detrital package is onlapped by high amplitude seismic reflectors overlain by the “Messinian Salt” and the “Upper Evaporites”. Towards the shelf, the transition between regressive deposits and overlying onlapping sediments is characterised by a wave-ravinement surface, suggesting that a significant part of the onlapping reflectors and overlying Messinian Evaporites were deposited during a relatively slow landward migration of the shoreline. The clear boundary between the smooth wave-ravinement surface and the subaerial Messinian Erosional Surface observed on the Gulf of Lions shelf and onshore in the Rhône valley is interpreted to have resulted from a rapid acceleration of the Mediterranean sea level rise at the end of the Messinian Salinity Crisis. Numerical simulation of this cycle of sea level change during the Messinian Salinity Crisis and of precipitation of thick evaporites during the slow sea level rise shows that this scenario can be modelled assuming a value of evaporation minus precipitation of 1.75 m3/m2/yr in the deep Mediterranean basins.
PY 2015
PD SEP
SO Marine And Petroleum Geology
SN 0264-8172
PU Elsevier Sci Ltd
VL 66
UT 000365055800017
BP 262
EP 277
DI 10.1016/j.marpetgeo.2014.12.013
ID 35887
ER

EF