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The Nd and Hf isotopic evolution of the mantle through the Archean. results from the Isua supracrustals, West Greenland, and from the Birimian terranes of West Africa

✍ Scribed by Janne Blichert-Toft; Francis Albarède; Minik Rosing; Robert Frei; David Bridgwater

No coin nor oath required. For personal study only.

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