Structural control of alkaline-ultrabasic magmatism in the north of Middle Siberia
Authors:
Abstract
Alkaline-ultrabasic magmatic manifestations in the north of Middle Siberia are known in the northern marginal part of the Siberian Platform and in the south of the Taimyr folded region. These manifestations of magmatism, confined to two different geostructural zones, are separated by the Yenisei-Khatanga trough. Alkaline-ultrabasic magmatism developed in parallel with trap magmatism during the formation of the Upper Paleozoic-Mesozoic structural stage.
Область исследования:
(Archived) Without section
Funding:
None
References
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