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This study analyzes 33 peridotite xenoliths from the Somerset Island kimberlite field, focusing on their Re–Os isotopic compositions and platinum-group elements (PGE). Results indicate that the cratonic lithosphere of Somerset Island stabilized at least 2.8 billion years ago, with evidence of Archean origins supported by mineralogy and thermobarometry. The findings also highlight differences in age and PGE patterns compared to the Slave and Kaapvaal cratons, suggesting complex geological processes in the re

Author

no2owl977

Language

EN