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- > Reconstructing ice-sheet dynamics from subglacial sediments and landforms. Special issue (supprimer)
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Par Collection Par Auteur- Ó COFAIGH, C., (Editeur scientifique) (3)
- DOWDESWELL, J.A. (1)
- EVANS, J. (1)
- GRAESCH, M. (1)
- HOOYER, T.S. (1)
- KLEMAN, J. (1)
- LARTER, R.D. (1)
- SHUMWAY, J.R. (1)
- THOMASON, J.F. (1)
- DE ANGELIS, H. (1)
- IVERSON, N.R. (1)
- Ó COFAIGH, C. (1)
- 2008 (3)
- Antarctica ; Bathymetry ; Conceptual model ; Continental shelf ; Deglaciation ; Geomorphology ; Geophysics ; Glacial features ; Ice sheet ; Pleistocene ; Sedimentology (1)
- Antarctique ; Bathymétrie ; Calotte glaciaire ; Déglaciation ; Glaciaire ; Géomorphologie ; Géophysique ; Modèle conceptuel ; Plate-forme continentale ; Pléistocène ; Sédimentologie (1)
- Arctic Region ; Baffin Land ; Canada ; Cold area ; Geographical information system ; Glacial features ; Ice sheet ; LANDSAT ; Moraine ; Northwest Territories ; Palaeogeography ; Remote sensing ; Thematic Mapper (1)
- Arctique ; Baffin Land ; Calotte glaciaire ; Canada ; Glaciaire ; LANDSAT ; Moraine ; Northwest Territories ; Paléoglaciologie ; Paléogéographie ; Système d'information géographique ; Thematic Mapper ; Télédétection ; Zone froide (1)
- Contrainte de cisaillement ; Ecoulement glaciaire ; Glaciaire ; Lithologie ; Modèle ; Moraine ; Susceptibilité magnétique (1)
- Glacial features ; Glacial flow ; Lithology ; Magnetic susceptibility ; Model ; Moraine ; Shear stress (1)
- Reconstructing ice-sheet dynamics from subglacial sediments and landforms. Special issue (3)
- Geological constraints on Antarctic palaeo-ice-stream retreat (1)
- Palaeo-ice-stream onsets : examples from the north-eastern Laurentide Ice Sheet (1)
- The experimental basis for interpreting particle and magnetic fabrics of sheared till (1)
- Geological constraints on Antarctic palaeo-ice-stream retreat
- are inferred from the geological evidence : rapid, episodic and slow. They indicate that Antarctic palaeo-ice-streams did not respond uniformly to external forcing at the end of the last glacial cycle. Rather, their diachronous retreat reflects the dominance
- This paper is aimed at exploring whether there is a simple, reproducible relationship between fabric development and shear-strain magnitude that could be used to help test the bed-deformation model using the geologic record. Four basal tills
- of north-eastern Canada formerly covered by the Laurentide Ice Sheet. Four different cases are considered and analysed in a geographical information system (GIS) environment with full integration of ancillary topographical and geological data. The AA