Abstract
The cataclasite and mylonites, and the brittle/ductile deformation processes that produced them, were studied in relation to the regional geology at exposures along the northern rim of the Grong culmination, a transverse basement antiform in the Scandinavian Caledonides.
| Original language | English |
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| Qualification | Doctor of Philosophy |
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| Supervisors/Advisors |
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| Award date | 11 Dec 1984 |
| Place of Publication | Utrecht |
| Publisher | |
| Publication status | Published - 11 Dec 1984 |
Bibliographical note
Geologica Ultraiectina ; 27Keywords
- Grong Region
- Norway
- Mylonite
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