Mantle transect of the Karelian Craton from margin to core based on P-T data from garnet and clinopyroxene xenocrysts in kimberlites

Peridotitic garnet and clinopyroxene xenocrysts from the 1.2 Ga Lentiira-Kuhmo and the 760 Ma Kuusamo kimberlite fields, emplaced within the Central Karelian Craton, have been studied using major and trace element geochemistry to obtain information on the stratigraphy, compositional variability, and...

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Bibliographic Details
Published in:Bulletin of the Geological Society of Finland
Main Authors: M. Lehtonen, H. O'Brien
Format: Article in Journal/Newspaper
Language:English
Published: Geological Society of Finland 2009
Subjects:
Online Access:https://doi.org/10.17741/bgsf/81.2.001
https://doaj.org/article/2b93532cb84b4c688cfbfc2106af9fee