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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Format: | Article in Journal/Newspaper |
Language: | English |
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1959
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Online Access: | https://hdl.handle.net/11250/2674693 |