The Geology of the Snøfjella and Dovrefjella in Vestspitsbergen
Abstract The area yields marbles, schists, and quartzites, probably of Hecla Hoek age, a series similar in lithology to those in the Kongsfjorden region. Their structure and metamorphic condition fit in with the general picture of Caledonian trend and of increasing orogenic activity westwards. Later...
Published in: | Geological Magazine |
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Main Author: | |
Format: | Article in Journal/Newspaper |
Language: | English |
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Cambridge University Press (CUP)
1959
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Online Access: | http://dx.doi.org/10.1017/s0016756800059203 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0016756800059203 |