Abstract
High-precision Hf isotopic analyses and U-Pb ages of carbonatites and kimberlites from Greenland and eastern North America, including Earth's oldest known carbonatite (3 Ga), indicate derivation from an enriched mantle source. This previously unidentified mantle reservoir-marked by an unradiogenic Hf isotopic composition and preserved in the deep mantle for at least 3 b.y.-may account for the mass imbalance in Earth's Hf-Nd budget. The Hf isotopic data presented here support a common mantle source region and genetic link between carbonatite and some oceanic-island basalt volcanoes.
Original language | English |
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Journal | Geology |
Volume | 30 |
Issue number | 9 |
Pages (from-to) | 771-774 |
Number of pages | 4 |
ISSN | 0091-7613 |
DOIs | |
Publication status | Published - 1 Sept 2002 |