M. Tesson et B. Gensous, TERNARY RECORD OF CLIMATIC AND EUSTATIC C YCLES ON MODERN MARGINS OF THE NORTH-MEDITERRANEAN BASIN, Comptes rendus de l'Academie des sciences. Serie II. Sciences de la terre et des planetes, 326(2), 1998, pp. 121-127
Studies of Quaternary deposits on shelves lead us to propose simplifie
d stratigraphic models, far from the global models, whose cyclic patte
rn is reduced to a regressive unit built up during a relative sea leve
l fall (cooling period). Analysis of neighbouring areas of the Gulf of
Lions show a more complex pattern. In the Languedoc area, the stratig
raphic model shows the record of falling stage, maximum lowstand, earl
y and late sea level rises. These attributes evolve laterally towards
the Rhone-Est and Ampurdan areas, into a simple model. Thus, Quaternar
y models are relevant to the global models and represent depending upo
n area, end members associated with the interaction of local factors a
nd global factors. (C) Academie des sciences/Elsevier, Paris.