The structure and cryptic layering of the Pados-Tundra ultramafic complex, Serpentinite belt, Kola Peninsula, Russia
The Paleoproterozoic Pados-Tundra ultramafic complex, ~6 x 1.5-2.1 km in size and ~2.1 Ga in age, located in the Kola Peninsula of Russia, is the main representative of the Serpentinite belt in the northern Fennoscandian Shield. It is composed of fragmented or foliated bodies of dunite-harzburgite-o...
| Published in: | Bulletin of the Geological Society of Finland |
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| Main Authors: | , , |
| Format: | Article in Journal/Newspaper |
| Language: | English |
| Published: |
Geological Society of Finland
2017
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| Subjects: | |
| Online Access: | https://doi.org/10.17741/bgsf/89.1.003 https://doaj.org/article/f9a44a83ddc14392af3f1d696fbaca9f |