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(Article of periodic en Anglais - 1989)

Document title

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

Authors(s) and Affiliation(s)

ANDREASSON P. G. ; GEE D. G. ;

Abstract

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

Source

Article of periodic

published at : Geografiska annaler. Series A. Physical geography / ISSN 0435-3676 / CODEN GAPGAP

Editor : Svenska sällskapet för antropologi och geografi, Stockholm - SUEDE (1965)

Millesime : 1989, vol. 71, no3-4 [pp. 235-239]

Bibliographic references : 11 réf.

Language

Anglais

Localisation

Centre national de la recherche scientifique

INIST-CNRS, Cote INIST : 2704 A

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