Metamorphism within the Çokkul synform: evidence for detachment faulting within the metamorphic infrastructure of the Norwegian Caledonides (67°30′N)
Within the Çokkul synform, Caledonian metamorphic rocks of the Middle Köli Nappe Complex (MKNC) are in low‐angle fault contact with the basement mylonites derived from the Precambrian Tysfjord granite‐gneiss. In the synform, the MKNC is composed of four fault‐bounded nappes each of which has a disti...
| Published in: | Journal of Metamorphic Geology |
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| Main Author: | |
| Format: | Article in Journal/Newspaper |
| Language: | English |
| Published: |
Wiley
1990
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| Online Access: | http://dx.doi.org/10.1111/j.1525-1314.1990.tb00491.x https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1525-1314.1990.tb00491.x https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1525-1314.1990.tb00491.x |