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This study presents U-Pb zircon geochronology from the Haag Nunataks gneiss complex in West Antarctica, revealing the ages of significant magmatic events at 1238 ± 4 Ma, 1064 ± 4 Ma, and 1056 ± 8 Ma. The findings suggest that the Haag Nunataks rocks are part of a juvenile arc setting related to the Grenville orogeny and provide insights into the tectonic history of the region in the context of Rodinia reconstructions. Additionally, correlations with other regions such as the Shackleton Range and Coats Land

Author

tamara.handl05

Language

EN