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...

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Bibliographic Details
Main Authors: Olesen, Odleiv, Solli, Arne
Format: Article in Journal/Newspaper
Language:English
Published: 1985
Subjects:
Online Access:https://hdl.handle.net/11250/2674249