Mechanism of Mineral Reactions Inferred from Textures of Impure Dolomitic Marbles from East Greenland
Mineral assemblages and chemical compositions of minerals found in impure dolomitic marbles embedded in gneisses and migmatites of the E. Greenland Caledonian fold belt (Scoresby Sund) suggest that the marbles were metamorphosed near 630 °C at 5 kb pressure. The analysis of complex textural and mine...
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| Language: | English |
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2017
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| Online Access: | http://doc.rero.ch/record/289380/files/23-3-325.pdf |