Geologiske undersøkelser i sørlige Helgeland og nordlige Namdal.
Cambro-Silurian rocks with large intrusive masses cover most of the area. In the south-westernmost part there are also deeper lying rocks. This part is referred to as the basal gneiss region, while the rest of the area is called the Nordland syncline. In the basal gneiss region there are 3 distinct...
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| Format: | Article in Journal/Newspaper |
| Language: | Norwegian |
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1967
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| Online Access: | https://hdl.handle.net/11250/2674890 |