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Multi-stage origin of the lower crust of the Karelian craton from 3.5 to 1.7 Ga based on isotopic ages of kimberlite-derived mafic granulite xenoliths

✍ Scribed by Petri Peltonen; Irmeli Mänttäri; Hannu Huhma; Martin J. Whitehouse


Book ID
116845506
Publisher
Elsevier Science
Year
2006
Tongue
English
Weight
747 KB
Volume
147
Category
Article
ISSN
0301-9268

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