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.
Originalsprog | Engelsk |
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Tidsskrift | Geology |
Vol/bind | 30 |
Udgave nummer | 9 |
Sider (fra-til) | 771-774 |
Antal sider | 4 |
ISSN | 0091-7613 |
DOI | |
Status | Udgivet - 1 sep. 2002 |