Arctic–alpine blockfields in the northern Swedish Scandes: late Quaternary – not Neogene
Autochthonous blockfield mantles may indicate alpine surfaces that have not been glacially eroded. These surfaces may therefore serve as markers against which to determine Quaternary erosion volumes in adjacent glacially eroded sectors. To explore these potential utilities, chemical weathering featu...
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| Principais autores: | , , , , , , |
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| Formato: | Artigo |
| Idioma: | Inglês |
| Publicado: |
Copernicus Publications
2014-07-01
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| Series: | Earth Surface Dynamics |
| Acceso en liña: | http://www.earth-surf-dynam.net/2/383/2014/esurf-2-383-2014.pdf |
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