Aillikites and Alkali Ultramafic Lamprophyres of the Beloziminsky Alkaline Ultrabasic-Carbonatite Massif: Possible Origin and Relations with Ore Deposits

Aillikites and Alkali Ultramafic Lamprophyres of the Beloziminsky Alkaline Ultrabasic-Carbonatite Massif: Possible Origin and Relations with Ore Deposits

The 650–621 Ma plume which impinged beneath the Siberian craton during the breakup of Rodinia caused the formation of several alkaline carbonatite massifs in craton margins of the Angara rift system. The Beloziminsky alkaline ultramafic carbonatite massif (BZM) in the Urik-Iya graben includes alnöit...

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Bibliographic Details
Main Authors: Igor Ashchepkov, Sergey Zhmodik, Dmitry Belyanin, Olga N. Kiseleva, Nikolay Medvedev, Alexei Travin, Denis Yudin, Nikolai S. Karmanov, Hilary Downes
Format: Article
Language:English
Published: MDPI AG 2020-04-01
Series:Minerals
Subjects:
carbonatite aillikites
mantle
rare metals
metasomatism
subduction
plume
Online Access:https://www.mdpi.com/2075-163X/10/5/404

Internet

https://www.mdpi.com/2075-163X/10/5/404

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