The alkaline complex of the Breivikbotn area, Sørøy, Northern Norway.
The alkaline rocks of the Breivikbotn area have been emplaced into highly folded and metamorphosed igneous and sedimentary rocks during the period of the Caledonian orogeny. They form an integral part of the complicated sequence of plutonic events that occurred during the orogeny, and were broadly s...
Main Authors: | , |
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Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
1965
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Subjects: | |
Online Access: | https://hdl.handle.net/11250/2674814 |