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Quantification des flux sédimentaires et de la subsidence du bassin ...

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tel-00790852, version 1 - 21 Feb 2013<br />

1059<br />

1060<br />

1061<br />

1062<br />

1063<br />

1064<br />

1065<br />

1066<br />

Variation of sea level is in blue and that of water budg<strong>et</strong> in b<strong>la</strong>ck. The resulting simu<strong>la</strong>tion of<br />

evaporite thickness is in purple. Solid and dashed lines are constrained by the initial position<br />

of the paleoshoreline just before step 2-III, respectively at 600 m and 900 m below the present<br />

sea level (Bache <strong>et</strong> al., 2012). The geom<strong>et</strong>ry of the basins is i<strong>de</strong>ntical to that previously used<br />

by (Meijer and Krijgsman, 2005). Evaporites begin to precipitate when water salinity reaches<br />

130g/l (Gargani <strong>et</strong> al., 2008; Meijer and Krijgsman, 2005). The water budg<strong>et</strong> is calcu<strong>la</strong>ted<br />

using river and At<strong>la</strong>ntic Ocean flow as well as precipitation and evaporation (Gargani and<br />

Rigoll<strong>et</strong>, 2007). See the supplementary materials for further d<strong>et</strong>ails.<br />

44

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