Fingerprints of Kamafugite-Like Magmas in Mesozoic Lamproites of the Aldan Shield: Evidence from Olivine and Olivine-Hosted Inclusions

Mesozoic (125–135 Ma) cratonic low-Ti lamproites from the northern part of the Aldan Shield do not conform to typical classification schemes of ultrapotassic anorogenic rocks. Here we investigate their origins by analyzing olivine and olivine-hosted inclusions from the Ryabinoviy pipe, a well preser...

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Bibliographic Details
Main Authors: Ivan F. Chayka, Alexander V. Sobolev, Andrey E. Izokh, Valentina G. Batanova, Stepan P. Krasheninnikov, Maria V. Chervyakovskaya, Alkiviadis Kontonikas-Charos, Anton V. Kutyrev, Boris M. Lobastov, Vasiliy S. Chervyakovskiy
Format: Article
Language:English
Published: MDPI AG 2020-04-01
Series:Minerals
Subjects:
Online Access:https://www.mdpi.com/2075-163X/10/4/337