Abstract. - The study of the fluviatile deposits remaining in the valleys of Western Brittany has shown that they generally must be interpreted as climatic terraces related to cold periods. Eustatic interglacial fluviatile terraces seem to have been poorly developed and are apparently not preserved, so that only some old estuarine eustatic sediments have been found.Résumé. - L'examen des dépôts fluviatiles conservés dans les vallées de Bretagne Occidentale a montré qu'ils correspondent pour la plupart à des terrasses climatiques froides. Les terrasses eustatiques fluviatiles interglaciaires, sans doute peu développées à l'origine, ne semblent pas s'être conservées, et pour l'instant seuls de dépôts fluvio-estuariens ont été reconnus.Hallégo...
Pedosedimentological study of the transitional formations existing between the Last Interglacial and...
Sedimentary and erosional phases responsible for the formation of fluviatile terraces are studied in...
Abstract. - The Somme valley, which began to take shape in pre-Tertiary times, consists of an axial ...
International audienceThe study of the fluviatile deposits remaining in the valleys of Western Britt...
The studies realized in Aquitaine and in the basin of Allier show a high correlation between paleocl...
SUMMARY Surveys carried out to the north of Angers, on the lower courses of the Sarthe and the Loir...
Loamy deposits along the northern coast of Brittany that correspond with periods of climatic deterio...
The typical sequence of the lower terrace of Somme valley at Longpré-les-Corps-Saints (Somme) shows ...
The coast of Tregor (North Brittany, France) displays many evidences of high quaternary sea levels. ...
On the western coast of Corsica, some sections are described, showing fluvial deposits passing later...
At Landerneau, the upper reaches of the Elorn estuary are filled with manne, fluviatile and penglaci...
At Roc-en-Pail, 130 km above the mouth of the Loire, a succession of loessic layers is well dated th...
Marine sediments lie at 20 m above present sea-level in the valley of the Elorn at Landerneau (Finis...
The foreland of Savoie shows three fluvio-glacial complexes. Two are convered by the « würmian » mor...
The vast synclinal of Val de Lans is filled in with a thick lacustrine and marsh formation whose dep...
Pedosedimentological study of the transitional formations existing between the Last Interglacial and...
Sedimentary and erosional phases responsible for the formation of fluviatile terraces are studied in...
Abstract. - The Somme valley, which began to take shape in pre-Tertiary times, consists of an axial ...
International audienceThe study of the fluviatile deposits remaining in the valleys of Western Britt...
The studies realized in Aquitaine and in the basin of Allier show a high correlation between paleocl...
SUMMARY Surveys carried out to the north of Angers, on the lower courses of the Sarthe and the Loir...
Loamy deposits along the northern coast of Brittany that correspond with periods of climatic deterio...
The typical sequence of the lower terrace of Somme valley at Longpré-les-Corps-Saints (Somme) shows ...
The coast of Tregor (North Brittany, France) displays many evidences of high quaternary sea levels. ...
On the western coast of Corsica, some sections are described, showing fluvial deposits passing later...
At Landerneau, the upper reaches of the Elorn estuary are filled with manne, fluviatile and penglaci...
At Roc-en-Pail, 130 km above the mouth of the Loire, a succession of loessic layers is well dated th...
Marine sediments lie at 20 m above present sea-level in the valley of the Elorn at Landerneau (Finis...
The foreland of Savoie shows three fluvio-glacial complexes. Two are convered by the « würmian » mor...
The vast synclinal of Val de Lans is filled in with a thick lacustrine and marsh formation whose dep...
Pedosedimentological study of the transitional formations existing between the Last Interglacial and...
Sedimentary and erosional phases responsible for the formation of fluviatile terraces are studied in...
Abstract. - The Somme valley, which began to take shape in pre-Tertiary times, consists of an axial ...