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PORTAIL D'INFORMATION GÉOGRAPHIQUE

Bedrock geology and morphology of the Tarfala area, Kebnekaise Mts., Swedish Caledonides

Auteurs :
ANDREASSON, P. G.
GEE, D. G.

Description :
In the Tarfala area, there are significant morphological differences between the different Seve Nappes, particularly between the dolerite dyke complexes and the underlying units consisting of amphibolites, gneisses and schists. The dolerites are often well preserved and the metasedimentary rocks are usually hard hornfelses. Other morphological breaks are caused by resistant mylonites along nappe boundaries, one prominent example occuring beneath Storglaciären.


Type de document :
Article de périodique

Source :
Geografiska annaler. Series A. Physical geography, issn : 0435-3676, 1989, vol. 71, n°. 3-4, p. 235-239, Références bibliographiques : 11 réf.

Date :
1989

Editeur :
Pays édition : Suede, Stockholm, Svenska sällskapet för antropologi och geografi

Langue :
Anglais
Droits :
Tous droits réservés © Prodig - Bibliographie Géographique Internationale (BGI)