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- > Special issue. Reconstruction and climatic implications of paleosols (supprimer)
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Par Collection Par Auteur- OLSEN, L. (1)
- STREMME, H.E. (1)
- VAN VLIET-LANOË, B. (1)
- 1998 (3)
- Corrélation stratigraphique ; Datation Th/U ; Europe ; Europe de l'Est ; France ; Interglaciaire ; Loess ; Moraine ; Normandie ; Paléosol ; Pays-Bas ; Pologne ; Propriétés du sol ; Quaternaire ; Stratigraphie ; Susceptibilité magnétique ; Tchèque, république ; Thermoluminescence ; Ukraine (1)
- Czech Republic ; Eastern Europe ; Europe ; France ; Interglacial ; Loess ; Magnetic susceptibility ; Moraine ; Netherlands (The) ; Normandie ; Palaeosol ; Poland ; Quaternary ; Soil properties ; Stratigraphic correlation ; Stratigraphy ; Th/U dating ; Thermoluminescence ; Ukraine (1)
- Erosion glaciaire ; Glaciaire ; Géochimie ; Norvège ; Paléoclimat ; Paléogéographie ; Paléosol ; Pléistocène ; Propriétés du sol ; Stratigraphie ; Susceptibilité magnétique (1)
- Geochemistry ; Glacial erosion ; Glacial features ; Magnetic susceptibility ; Norway ; Palaeoclimate ; Palaeogeography ; Palaeosol ; Pleistocene ; Soil properties ; Stratigraphy (1)
- Special issue. Reconstruction and climatic implications of paleosols (3)
- Correlation of Quaternary pedostratigraphy from western to eastern Europe (1)
- Frost and soils : implications for paleosols, paleoclimates and stratigraphy (1)
- Pleistocene paleosols in Norway : implications for past climate and glacial erosion (1)
- Czech Republic ; Eastern Europe ; Europe ; France ; Interglacial ; Loess ; Magnetic susceptibility ; Moraine ; Netherlands (The) ; Normandie ; Palaeosol ; Poland ; Quaternary ; Soil properties ; Stratigraphic correlation ; Stratigraphy ; Th/U dating
- by stratigraphic, magnetic and chemical methods. The presence of these buried Pleistocene paleosols in the interior of Norway (central part of the Fennoscandian glaciations) indicates that glacial erosion was locally less during several glacial cycles than
- Frost is a pedogenetic agent. This paper describes the use of frost features in soil for paleoclimatic and stratigraphic interpretation. It is possible to differentiate periods of frost activity from those of temperate pedogenesis by macroscopic