Hydrothermal processes in mylonitic rocks at the NW edge of the Grong culmination, central Norway
Publication date
1984-12-11
Authors
Stel, H.
Editors
Advisors
Supervisors
Zwart, H.J.
DOI
Document Type
Dissertation
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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.
Keywords
Grong Region, Norway, Mylonite
Citation
Stel, H 1984, 'Hydrothermal processes in mylonitic rocks at the NW edge of the Grong culmination, central Norway', Doctor of Philosophy, Universiteit Utrecht, Utrecht.