The Mesoproterozoic mantle plume beneath the northern part of the Siberian craton
The study of the Mesoproterozoic (1473 ± 24 Ma) dolerites of the Olenek uplift of the Siberian craton basement has shown their petrologic and geochemical similarity to typical OIB produced with participation of a mantle plume. The dolerites are characterized by variations in the geochemical composit...
| Main Authors: | Gladkochub, D., Donskaya, T., Mazukabzov, A., Pisarevskiy, Sergei, Ernst, R., Stanevich, A. |
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| Format: | Journal Article |
| Published: |
Elsevier BV
2016
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| Online Access: | http://hdl.handle.net/20.500.11937/53455 |
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