Evidence of Enriched, Hadean Mantle Reservoir from 4.2-4.0 Ga zircon xenocrysts from Paleoarchean TTGs of the Singhbhum Craton, Eastern India
Abstract Sensitive High-Resolution Ion Microprobe (SHRIMP) U-Pb analyses of zircons from Paleoarchean (~3.4 Ga) tonalite-gneiss called the Older Metamorphic Tonalitic Gneiss (OMTG) from the Champua area of the Singhbhum Craton, India, reveal 4.24-4.03 Ga xenocrystic zircons, suggesting that the OMTG...
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| Autores principales: | , , , , |
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| Formato: | article |
| Lenguaje: | EN |
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Nature Portfolio
2018
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| Acceso en línea: | https://doaj.org/article/6e0e88b058794af2a85adf332f9ff76c |
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