The Precambiran schists and gneisses of Lakselv valley, northern Norway.

The principal rocks of the Lakselv valley area are well-foliated hornblende schist and mica-quartz schists and lesser amounts of quartzite and marble. The hornblende schist overlies most of the mica-quartz schists and in several places is interlayered with them on a small scale. The structure of the...

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Bibliographic Details
Main Author: Crowder, Dwight F.
Format: Article in Journal/Newspaper
Language:English
Published: 1959
Subjects:
Online Access:https://hdl.handle.net/11250/2674693