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-Reference-Cited by-同舟云学术

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

Published:1999-11 Issue:22 Volume:63 Page:3901-3914
ISSN:0016-7037
Container-title:Geochimica et Cosmochimica Acta
language:en
Short-container-title:Geochimica et Cosmochimica Acta

Author:

Blichert-Toft Janne,Albarède Francis,Rosing Minik,Frei Robert,Bridgwater David

Publisher

Elsevier BV

Subject

Geochemistry and Petrology

Reference71 articles.

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3. The growth of continental crust;Albarède;Tectonophysics,1998

4. The geochemical regimes of Piton de la Fournaise volcano (Réunion) during the last 530000 years;Albarède;J. Petrol.,1997

5. The pre-3760 m.y. old supracrustal rocks of the Isua area, southern West Greenland, and the associated occurrence of quartz-banded ironstone;Allart,1976

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