Geophysical and geological interpretation of regional structures within the Precambrian Kautokeino Greenstone Belt, Finnmark, North Norway.
The Kautokeino Greenstone Belt comprises a synclinorium of volcano-sedimentary rocks. This sequence of Early Proterozoic age is situated between two culminations of gneisses. Large areas of the belt have been mapped in detail (1:50.000) and petrophysical properties of about 1150 rock samples have be...
Main Authors: | , |
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Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
1985
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Subjects: | |
Online Access: | https://hdl.handle.net/11250/2674249 |