Re-Os Isotope and HSE Abundance Systematics of the 2.9 Ga Komatiites and Basalts from the Sumozero-Kenozero Greenstone Belt, SE Fennoscandian Shield: Implications for the Mixing Rates of the Mantle-Reference-Cited by-同舟云学术

Re-Os Isotope and HSE Abundance Systematics of the 2.9 Ga Komatiites and Basalts from the Sumozero-Kenozero Greenstone Belt, SE Fennoscandian Shield: Implications for the Mixing Rates of the Mantle

Published:2022-11-15 Issue:6 Volume:30 Page:548-566
ISSN:0869-5911
Container-title:Petrology
language:en
Short-container-title:Petrology

Author:

Puchtel Igor S.

Publisher

Pleiades Publishing Ltd

Subject

Geochemistry and Petrology

Link

https://link.springer.com/content/pdf/10.1134/S0869591122060054.pdf

Reference94 articles.

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3. Becker, H., Horan, M.F., Walker, R.J., et al., Highly siderophile element composition of the Earth’s primitive upper mantle: constraints from new data on peridotite massifs and xenoliths, Geochim. Cosmochim. Acta, 2006, vol. 70, no. 17, pp. 4528–4550.

4. Birck, J.L., Roy-Barman, M., and Capman, F., Re-Os isotopic measurements at the femtomole level in natural samples, Geostand. Newslett., 1997, no. 1, pp. 19–27.

5. Blichert-Toft, J. and Puchtel, I.S., Depleted mantle sources through time: evidence from Lu–Hf and Sm-Nd isotope systematics of Archean komatiites, Earth Planet. Sci. Lett., 2010, vol. 297, nos. 3-4, pp. 598–606.

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