Fluid evolution during metamorphism at increasing pressure:carbonic- and nitrogen-bearing fluid inclusions in granulites from Øksfjord, north Norwegian Caledonides
Three successive metamorphic stages M1, M2 and M3 have been distinguished in polymetamorphic granulite facies quartz-feldspathic gneisses from the Seiland Igneous Province, Caledonides of northern Norway. An early period of contact metamorphism (M1; 750-950°C, ca. 5 kbar) was followed by cooling, ac...
| Published in: | Contributions to Mineralogy and Petrology |
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| Main Authors: | , |
| Format: | Article in Journal/Newspaper |
| Language: | English |
| Published: |
1993
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| Subjects: | |
| Online Access: | https://researchers.mq.edu.au/en/publications/23bf8c21-9ecd-4afb-afe2-b5e1bf68fd9b https://doi.org/10.1007/BF00307758 http://www.scopus.com/inward/record.url?scp=0027455210&partnerID=8YFLogxK |