Description of quaternary alluvial system of the Garonne. The low plain deposits, with brown-leached profiles, are Würm old. The low terrace, with hydromorphic leached soils in silt and already weathered deep horizons in alluvial pebbles, dates from the Riss period.Hubschman Jacques. II.— Les terrasses récentes de la Garonne et leur évolution. In: Bulletin de l'Association française pour l'étude du quaternaire, vol. 12, n°3-4, 1975. pp. 137-147
The Garonne Basin is the axial geomorphological entity of the Aquitain. In recent years, the middle ...
At Roc-en-Pail, 130 km above the mouth of the Loire, a succession of loessic layers is well dated th...
Civil Engineering Geology depends largely upon Quaternary Geology, which determines many important p...
Description of quaternary alluvial system of the Garonne. The low plain deposits, with brown-leached...
Description and analysis of the Garonne pre-Riss deposits. Mindel alluvial pebble weathering is show...
Soils and particularly weathering rocks data on alluvial gravels tends to assumption of a non-synchr...
The ancient studies of the alluvial deposits of the Têt (Pyrénées Orientales, France) are numerous. ...
Quaternary formations from the sub-pyrenean region get their origin from the reworking of former det...
Two bores were dug in the Garon Valley (SW of Lyon, France). They show clays under thick quaternary ...
The quaternary terraces from Roussillon plain in french Catalogne yielded several crude pebble-tools...
Conclusions concerning chiefly the soils and geochemical weathering studies in the Garonne Pyrenean ...
In Upper Normandy the Lower Pleistocene is made up of sands with pebble levels, and fersiallitic-typ...
After the deposit of würmian alluvium ("lower terrace" of 15-20 m), one can distinguish two phases o...
In the middle Durance valley, between the villages of Les Mées and Oraison, eight quaternary level t...
Nature and situation of pho-quaternary alluvial and aeolian formations in Touraine allow neither geo...
The Garonne Basin is the axial geomorphological entity of the Aquitain. In recent years, the middle ...
At Roc-en-Pail, 130 km above the mouth of the Loire, a succession of loessic layers is well dated th...
Civil Engineering Geology depends largely upon Quaternary Geology, which determines many important p...
Description of quaternary alluvial system of the Garonne. The low plain deposits, with brown-leached...
Description and analysis of the Garonne pre-Riss deposits. Mindel alluvial pebble weathering is show...
Soils and particularly weathering rocks data on alluvial gravels tends to assumption of a non-synchr...
The ancient studies of the alluvial deposits of the Têt (Pyrénées Orientales, France) are numerous. ...
Quaternary formations from the sub-pyrenean region get their origin from the reworking of former det...
Two bores were dug in the Garon Valley (SW of Lyon, France). They show clays under thick quaternary ...
The quaternary terraces from Roussillon plain in french Catalogne yielded several crude pebble-tools...
Conclusions concerning chiefly the soils and geochemical weathering studies in the Garonne Pyrenean ...
In Upper Normandy the Lower Pleistocene is made up of sands with pebble levels, and fersiallitic-typ...
After the deposit of würmian alluvium ("lower terrace" of 15-20 m), one can distinguish two phases o...
In the middle Durance valley, between the villages of Les Mées and Oraison, eight quaternary level t...
Nature and situation of pho-quaternary alluvial and aeolian formations in Touraine allow neither geo...
The Garonne Basin is the axial geomorphological entity of the Aquitain. In recent years, the middle ...
At Roc-en-Pail, 130 km above the mouth of the Loire, a succession of loessic layers is well dated th...
Civil Engineering Geology depends largely upon Quaternary Geology, which determines many important p...